ALMA will deliver exciting opportunities to advance our understanding of solar prominences and filaments, and constrain models of prominence fine structures.
This document summarizes a study that used wide-swath interferometric synthetic aperture radar (InSAR) time series to map large-scale ground deformation over the Danakil depression in the Afar region of Ethiopia between 2006 and 2009. The time series analysis revealed deformation signals consistent with magmatic intrusions and inflation/deflation of volcanic centers. Modeling of the deformation supported deep magma intrusion beneath the central segment and lateral magma propagation and chamber inflation beneath Dabbahu volcano in the northern segment. The study demonstrated the potential of wide-swath InSAR time series for mapping long-wavelength ground deformation over large areas.
- The document discusses methods for characterizing dark energy and modified gravity models in a model-independent way using cosmological observations.
- Due to the "dark degeneracy" between dark matter and dark energy, it is not possible to separately measure the properties of dark matter and dark energy without assuming a specific model class.
- Observables like the Hubble parameter H(z) and gravitational potentials can be reconstructed from the data, but this does not break the degeneracy between dark matter and dark energy contributions.
- The scale-dependence of quantities like the gravitational potentials and growth rate can be used to test and constrain broad classes of dark energy and modified gravity models in a more model-independent way.
Binary pulsars provide an excellent tool to test theories of gravity. The document describes several binary pulsar systems and how measurements of their orbital parameters over time have allowed for high-precision tests of general relativity in strong gravitational fields. Specifically, the double pulsar system PSR J0737-3039A/B has enabled measurements that agree with general relativity predictions to within 0.05% precision by measuring parameters like periastron advance and gravitational redshift effects.
The document summarizes initial measurements of mesospheric gravity waves over McMurdo, Antarctica using infrared imaging. Over 300 gravity wave events were observed and analyzed over the 2012 season. The observed horizontal wavelengths averaged 22 km, phase speeds averaged 53.3 m/s. Wave propagation directions varied seasonally, with northwest in fall, isotropic in winter, and southwest in spring. Comparisons show similar wave characteristics to other Antarctic sites, but McMurdo exhibits a wider range of phase speeds. Ongoing analysis will help understand pan-Antarctic gravity wave climatology.
This paper analyzes photographic observations of the 1995 Quadrantid meteor shower made by the Dutch Meteor Society. The orbits of 95 Quadrantid meteors were precisely measured from photographic plates, providing the highest accuracy orbital data yet for this stream. Analysis of the orbits shows that the dispersion is much less than previous studies, indicating that the main component of the Quadrantid stream is only about 500 years old, much younger than the 5000-7500 years assumed previously. This suggests that the main peak arises from a recent "outburst" rather than the classical dust component. The stream likely does not originate from comet 96P/Machholz 1 as thought, and its true parent body may be an asteroid-like object in a
The document discusses advances in SAR interferometry over the past 20 years for measuring millimeter-scale land motion. Key points include:
1) Revisit times have decreased from 35 days with ERS-1 to 12 days with Sentinel-1 constellations, improving ground motion recovery.
2) Persistent scatterer interferometry techniques like SqueeSAR can now measure motions to the millimeter by using all available interferograms.
3) Atmospheric phase screens still limit accuracy but can be estimated and removed using numerical weather models, GPS, and other independent datasets.
4) Future opportunities include using wide Doppler bandwidths from satellites to achieve high-resolution azimuth measurements of ground motion.
The Gravity Probe B experiment tested two predictions of general relativity using gyroscopes in a satellite orbiting Earth. It measured the geodetic precession and frame-dragging precession predicted by Einstein to within 0.2% and 18.4% accuracy, respectively, confirming his theory of gravitation. Technical challenges arose from the gyroscopes not being perfectly spherical, leading to greater errors than anticipated. The experiment was a decades-long effort involving NASA, Stanford University, and collaboration with other institutions.
This document summarizes a study that used wide-swath interferometric synthetic aperture radar (InSAR) time series to map large-scale ground deformation over the Danakil depression in the Afar region of Ethiopia between 2006 and 2009. The time series analysis revealed deformation signals consistent with magmatic intrusions and inflation/deflation of volcanic centers. Modeling of the deformation supported deep magma intrusion beneath the central segment and lateral magma propagation and chamber inflation beneath Dabbahu volcano in the northern segment. The study demonstrated the potential of wide-swath InSAR time series for mapping long-wavelength ground deformation over large areas.
- The document discusses methods for characterizing dark energy and modified gravity models in a model-independent way using cosmological observations.
- Due to the "dark degeneracy" between dark matter and dark energy, it is not possible to separately measure the properties of dark matter and dark energy without assuming a specific model class.
- Observables like the Hubble parameter H(z) and gravitational potentials can be reconstructed from the data, but this does not break the degeneracy between dark matter and dark energy contributions.
- The scale-dependence of quantities like the gravitational potentials and growth rate can be used to test and constrain broad classes of dark energy and modified gravity models in a more model-independent way.
Binary pulsars provide an excellent tool to test theories of gravity. The document describes several binary pulsar systems and how measurements of their orbital parameters over time have allowed for high-precision tests of general relativity in strong gravitational fields. Specifically, the double pulsar system PSR J0737-3039A/B has enabled measurements that agree with general relativity predictions to within 0.05% precision by measuring parameters like periastron advance and gravitational redshift effects.
The document summarizes initial measurements of mesospheric gravity waves over McMurdo, Antarctica using infrared imaging. Over 300 gravity wave events were observed and analyzed over the 2012 season. The observed horizontal wavelengths averaged 22 km, phase speeds averaged 53.3 m/s. Wave propagation directions varied seasonally, with northwest in fall, isotropic in winter, and southwest in spring. Comparisons show similar wave characteristics to other Antarctic sites, but McMurdo exhibits a wider range of phase speeds. Ongoing analysis will help understand pan-Antarctic gravity wave climatology.
This paper analyzes photographic observations of the 1995 Quadrantid meteor shower made by the Dutch Meteor Society. The orbits of 95 Quadrantid meteors were precisely measured from photographic plates, providing the highest accuracy orbital data yet for this stream. Analysis of the orbits shows that the dispersion is much less than previous studies, indicating that the main component of the Quadrantid stream is only about 500 years old, much younger than the 5000-7500 years assumed previously. This suggests that the main peak arises from a recent "outburst" rather than the classical dust component. The stream likely does not originate from comet 96P/Machholz 1 as thought, and its true parent body may be an asteroid-like object in a
The document discusses advances in SAR interferometry over the past 20 years for measuring millimeter-scale land motion. Key points include:
1) Revisit times have decreased from 35 days with ERS-1 to 12 days with Sentinel-1 constellations, improving ground motion recovery.
2) Persistent scatterer interferometry techniques like SqueeSAR can now measure motions to the millimeter by using all available interferograms.
3) Atmospheric phase screens still limit accuracy but can be estimated and removed using numerical weather models, GPS, and other independent datasets.
4) Future opportunities include using wide Doppler bandwidths from satellites to achieve high-resolution azimuth measurements of ground motion.
The Gravity Probe B experiment tested two predictions of general relativity using gyroscopes in a satellite orbiting Earth. It measured the geodetic precession and frame-dragging precession predicted by Einstein to within 0.2% and 18.4% accuracy, respectively, confirming his theory of gravitation. Technical challenges arose from the gyroscopes not being perfectly spherical, leading to greater errors than anticipated. The experiment was a decades-long effort involving NASA, Stanford University, and collaboration with other institutions.
This document summarizes a study of mesospheric gravity waves over McMurdo Station, Antarctica using infrared imaging:
1) Over 400 short-period gravity waves were observed between March-September 2012, with average horizontal wavelength of 22 km, phase speed of 42 m/s, and period of 12 minutes.
2) Waves exhibited seasonal variations in propagation direction, with northwest in fall expanding to northeast and southwest in winter and more isotropic propagation in late winter.
3) Analysis of 73 continuous hours in June revealed over 40 gravity wave events with characteristics consistent with full season results. Diurnal and semidiurnal tides were also observed.
4) Later season observations in August showed higher average phase
The document discusses refraction seismology field work. It covers types of seismometers used, how a refraction survey is set up with geophone spreads and shot locations, and controlled seismic sources like impact and vibrating sources. An example refraction profile from Santa Teresa Hills is shown and discussed, including determining intercept times and velocities to develop a geophysical model of subsurface layers. Students are assigned a field study report on their refraction data due next month.
1) Geophysics uses remote sensing to determine subsurface conditions by analyzing seismic and radar signals that travel through and reflect off underground materials.
2) There are four main modes of signal propagation: vertical reflection, wide angle reflection, critical refraction, and direct waves. Precisely measuring the travel times of these signals allows subsurface structures to be interpreted.
3) Reflection seismology analyzes reflected signals to determine depth to interfaces by relating travel time, distance between source and receiver, and velocity, while refraction seismology uses travel times of critically refracted signals to determine shallow subsurface velocity structure.
Locating a satellite precisely is important for altimetry data quality. The Doris system uses the Doppler effect to determine a satellite's position by calculating the difference between emitted and received signal frequencies from ground beacons. Precise orbit determination requires processing measurements over time while accounting for forces like gravity, as the accuracy improves from 10 cm after 3 hours to 2.5 cm after 30 days. Doris positioning can also locate ground beacons outside the reference network for temporary monitoring of objects like volcanoes.
The document discusses several types of seismic velocity models including 1D layered models, community velocity models based on direct measurements, unified community models, and 3D tomography models derived from active and passive seismic data. It provides details on numerous global and regional reference models for the crust, mantle, and specific tectonic provinces.
The document discusses seismic reflection acquisition, processing, and waveform analysis. It provides examples of a large seismic data acquisition project in Saudi Arabia that collected over 120 million traces. It also defines key concepts in seismic processing like normal moveout correction, velocity analysis, muting, static corrections, average velocity, root mean square velocity, and interval velocity. It notes that the mid-term exam will be on May 3rd and that a field trip is scheduled for April 26th.
The document provides an overview of principles of seismic data interpretation. It discusses fundamentals of seismic acquisition and processing such as seismic response, phase, polarity, reflections, and resolution. It also covers topics like structural interpretation pitfalls, seismic interpretation workflows involving building databases and time-depth relationships, and structural styles. The document includes sections on depth conversion, subsurface mapping techniques, and different types of velocities.
This document outlines the key steps in a simple seismic data processing workflow, including: data initialization such as reformatting, geometry updates, and trace editing; amplitude processing; noise attenuation; deconvolution; multiple attenuation; velocity analysis and NMO; migration; stacking; and data makeup. Each processing step is briefly described and examples are provided of before and after visualizations. References and an opportunity for questions are provided at the end.
IOSR Journal of Applied Physics (IOSR-JAP) is an open access international journal that provides rapid publication (within a month) of articles in all areas of physics and its applications. The journal welcomes publications of high quality papers on theoretical developments and practical applications in applied physics. Original research papers, state-of-the-art reviews, and high quality technical notes are invited for publications.
1) Seismic interpretation uses acoustic waves to image the subsurface by measuring the two-way travel time and amplitude of reflections. 2) A seismic source generates wavefronts that travel through the subsurface, reflecting or transmitting at interfaces between rock layers. 3) The amount of reflection depends on the relative difference in physical properties across interfaces, defined by reflection coefficients. Layers thinner than 1/4 the wavelength cannot be resolved individually.
A dust-enshrouded tidal disruption event with a resolved radio jet in a galax...Sérgio Sacani
Tidal disruption events (TDEs) are transient flares produced when a star is ripped apart by the
gravitational field of a supermassive black hole (SMBH). We have observed a transient source in the
western nucleus of the merging galaxy pair Arp 299 that radiated >1.5 × 1052 erg in the infrared and radio
but was not luminous at optical or x-ray wavelengths. We interpret this as a TDE with much of its emission
reradiated at infrared wavelengths by dust. Efficient reprocessing by dense gas and dust may explain the
difference between theoretical predictions and observed luminosities of TDEs. The radio observations
resolve an expanding and decelerating jet, probing the jet formation and evolution around a SMBH.
Seismic data Interpretation On Dhodak field PakistanJamal Ahmad
I (Jamal Ahmad) presented this on 21 Feb, 2009 to defend my M.Phil dissertation in Geophysics at QAU, Islamabad, Pakistan. For more information about this, you may contact me directly at jamal.qau@gmail.com.
The 21cm line from neutral hydrogen can be used to study cosmology during the first billion years of the universe. This includes the Dark Ages when no structures formed, the Cosmic Dawn when the first luminous objects formed, and the Epoch of Reionization when these objects reionized the intergalactic medium. Current and future 21cm experiments like LOFAR, MWA, PAPER, and HERA aim to detect the signal from these eras but face challenges in calibrating the instruments and subtracting bright foreground sources. Some progress has been made in placing upper limits on the signal and constraining the heating of the intergalactic medium by X-rays, but a clear detection of the signal is still needed
The document discusses seismic reflection acquisition, processing, and waveform analysis. It introduces key concepts in seismic reflection including common midpoint gathers, common depth point gathers, and normal moveout correction. The document also discusses equipment used in land and marine seismic reflection acquisition such as vibrator trucks, geophones, and receiver trucks. It notes that processing aims to enhance the quality of compressional waves and improve the signal-to-noise ratio through techniques like stacking traces.
This document discusses using future full-sky galaxy surveys from space telescopes to probe initial conditions and constrain primordial non-Gaussianity. It proposes launching a space telescope called SPHEREx to conduct a full-sky galaxy spectroscopy survey. This would allow probing the horizon-scale clustering needed to constrain the non-Gaussianity parameter fNL using both the galaxy power spectrum and bispectrum. Current forecasts suggest SPHEREx could achieve an uncertainty of σ(fNL) ~ 0.8 from the power spectrum alone and σ(fNL) ~ 0.2 when also including the bispectrum. However, challenges remain in applying photometric redshift indicators and understanding contributions to the squeezed bispectrum at higher orders.
1) The document discusses which seismic attributes are most useful for quantitative seismic reservoir characterization. It analyzes attributes such as zero phase amplitude, relative impedance, and absolute impedance.
2) The conclusion is that an absolute impedance inversion provides the best attribute in theory but is difficult in practice. A relative impedance inversion, which is easier to generate, works nearly as well for characterization.
3) Key advantages of relative impedance over zero phase amplitude include relating to geology rather than just impedance contrasts, and allowing comparison between seismic datasets and well logs after appropriate scaling. However, relative impedance lacks low frequency content included in absolute impedance.
This document discusses static correction in seismic data processing. It covers:
1) Static correction removes the effects of surface elevation changes and weathering layers on seismic data.
2) Examples are given of how water depth variations can induce pull-down of reflectors, though this does not represent real geology.
3) A figure from a research paper shows a seismic section with associated velocity information, geology, and an approximate static corrections diagram.
This is for student of geophysics who want to know about basic of multi component seismic. For further detail or any query you can drop me mail, my mail id id bprasad461@gmail.com
This document summarizes experiments demonstrating synthetic aperture radar interferometry (InSAR) using the TerraSAR-X and TanDEM-X satellites under crossing orbits. The experiments showed that InSAR is feasible with crossing orbits if small squints are applied. Repeat-pass InSAR acquisitions under large crossing angles also produced coherent fringes, enabling 1, 5, and 6 day repeats. Time series analysis of the Ronne Ice Shelf in Antarctica exploited the rapidly varying baselines between acquisitions to study ice shelf velocity gradients and decorrelation effects.
This document summarizes a study that used wide-swath interferometric synthetic aperture radar (InSAR) time series to map large-scale ground deformation over the Danakil depression in the Afar region of Ethiopia between 2006 and 2009. The time series analysis revealed deformation signals consistent with magmatic intrusions and inflation/deflation of volcanic centers. Modeling of the deformation supported deep magma intrusion beneath the central segment and lateral magma propagation and chamber inflation beneath Dabbahu volcano in the northern segment. The study demonstrated the potential of wide-swath InSAR time series for mapping long-wavelength ground deformation over large areas.
This document summarizes a study examining the hypergiant star ρ Cassiopeiae. The researchers developed a model to explain ρ Cassiopeiae's variable mass loss rate, high microturbulent velocity, and Hα emission line profile using a stochastic field of shock waves in the star's atmosphere. Their model successfully reproduced the observed mass loss rate, microturbulent velocity, and aspects of the Hα profile using only one parameter - the maximum Mach number of shock waves in the atmosphere. The model indicates that thin, hot regions behind shock waves are responsible for the observed microturbulence and contribute to Hα emission.
This document summarizes a study of mesospheric gravity waves over McMurdo Station, Antarctica using infrared imaging:
1) Over 400 short-period gravity waves were observed between March-September 2012, with average horizontal wavelength of 22 km, phase speed of 42 m/s, and period of 12 minutes.
2) Waves exhibited seasonal variations in propagation direction, with northwest in fall expanding to northeast and southwest in winter and more isotropic propagation in late winter.
3) Analysis of 73 continuous hours in June revealed over 40 gravity wave events with characteristics consistent with full season results. Diurnal and semidiurnal tides were also observed.
4) Later season observations in August showed higher average phase
The document discusses refraction seismology field work. It covers types of seismometers used, how a refraction survey is set up with geophone spreads and shot locations, and controlled seismic sources like impact and vibrating sources. An example refraction profile from Santa Teresa Hills is shown and discussed, including determining intercept times and velocities to develop a geophysical model of subsurface layers. Students are assigned a field study report on their refraction data due next month.
1) Geophysics uses remote sensing to determine subsurface conditions by analyzing seismic and radar signals that travel through and reflect off underground materials.
2) There are four main modes of signal propagation: vertical reflection, wide angle reflection, critical refraction, and direct waves. Precisely measuring the travel times of these signals allows subsurface structures to be interpreted.
3) Reflection seismology analyzes reflected signals to determine depth to interfaces by relating travel time, distance between source and receiver, and velocity, while refraction seismology uses travel times of critically refracted signals to determine shallow subsurface velocity structure.
Locating a satellite precisely is important for altimetry data quality. The Doris system uses the Doppler effect to determine a satellite's position by calculating the difference between emitted and received signal frequencies from ground beacons. Precise orbit determination requires processing measurements over time while accounting for forces like gravity, as the accuracy improves from 10 cm after 3 hours to 2.5 cm after 30 days. Doris positioning can also locate ground beacons outside the reference network for temporary monitoring of objects like volcanoes.
The document discusses several types of seismic velocity models including 1D layered models, community velocity models based on direct measurements, unified community models, and 3D tomography models derived from active and passive seismic data. It provides details on numerous global and regional reference models for the crust, mantle, and specific tectonic provinces.
The document discusses seismic reflection acquisition, processing, and waveform analysis. It provides examples of a large seismic data acquisition project in Saudi Arabia that collected over 120 million traces. It also defines key concepts in seismic processing like normal moveout correction, velocity analysis, muting, static corrections, average velocity, root mean square velocity, and interval velocity. It notes that the mid-term exam will be on May 3rd and that a field trip is scheduled for April 26th.
The document provides an overview of principles of seismic data interpretation. It discusses fundamentals of seismic acquisition and processing such as seismic response, phase, polarity, reflections, and resolution. It also covers topics like structural interpretation pitfalls, seismic interpretation workflows involving building databases and time-depth relationships, and structural styles. The document includes sections on depth conversion, subsurface mapping techniques, and different types of velocities.
This document outlines the key steps in a simple seismic data processing workflow, including: data initialization such as reformatting, geometry updates, and trace editing; amplitude processing; noise attenuation; deconvolution; multiple attenuation; velocity analysis and NMO; migration; stacking; and data makeup. Each processing step is briefly described and examples are provided of before and after visualizations. References and an opportunity for questions are provided at the end.
IOSR Journal of Applied Physics (IOSR-JAP) is an open access international journal that provides rapid publication (within a month) of articles in all areas of physics and its applications. The journal welcomes publications of high quality papers on theoretical developments and practical applications in applied physics. Original research papers, state-of-the-art reviews, and high quality technical notes are invited for publications.
1) Seismic interpretation uses acoustic waves to image the subsurface by measuring the two-way travel time and amplitude of reflections. 2) A seismic source generates wavefronts that travel through the subsurface, reflecting or transmitting at interfaces between rock layers. 3) The amount of reflection depends on the relative difference in physical properties across interfaces, defined by reflection coefficients. Layers thinner than 1/4 the wavelength cannot be resolved individually.
A dust-enshrouded tidal disruption event with a resolved radio jet in a galax...Sérgio Sacani
Tidal disruption events (TDEs) are transient flares produced when a star is ripped apart by the
gravitational field of a supermassive black hole (SMBH). We have observed a transient source in the
western nucleus of the merging galaxy pair Arp 299 that radiated >1.5 × 1052 erg in the infrared and radio
but was not luminous at optical or x-ray wavelengths. We interpret this as a TDE with much of its emission
reradiated at infrared wavelengths by dust. Efficient reprocessing by dense gas and dust may explain the
difference between theoretical predictions and observed luminosities of TDEs. The radio observations
resolve an expanding and decelerating jet, probing the jet formation and evolution around a SMBH.
Seismic data Interpretation On Dhodak field PakistanJamal Ahmad
I (Jamal Ahmad) presented this on 21 Feb, 2009 to defend my M.Phil dissertation in Geophysics at QAU, Islamabad, Pakistan. For more information about this, you may contact me directly at jamal.qau@gmail.com.
The 21cm line from neutral hydrogen can be used to study cosmology during the first billion years of the universe. This includes the Dark Ages when no structures formed, the Cosmic Dawn when the first luminous objects formed, and the Epoch of Reionization when these objects reionized the intergalactic medium. Current and future 21cm experiments like LOFAR, MWA, PAPER, and HERA aim to detect the signal from these eras but face challenges in calibrating the instruments and subtracting bright foreground sources. Some progress has been made in placing upper limits on the signal and constraining the heating of the intergalactic medium by X-rays, but a clear detection of the signal is still needed
The document discusses seismic reflection acquisition, processing, and waveform analysis. It introduces key concepts in seismic reflection including common midpoint gathers, common depth point gathers, and normal moveout correction. The document also discusses equipment used in land and marine seismic reflection acquisition such as vibrator trucks, geophones, and receiver trucks. It notes that processing aims to enhance the quality of compressional waves and improve the signal-to-noise ratio through techniques like stacking traces.
This document discusses using future full-sky galaxy surveys from space telescopes to probe initial conditions and constrain primordial non-Gaussianity. It proposes launching a space telescope called SPHEREx to conduct a full-sky galaxy spectroscopy survey. This would allow probing the horizon-scale clustering needed to constrain the non-Gaussianity parameter fNL using both the galaxy power spectrum and bispectrum. Current forecasts suggest SPHEREx could achieve an uncertainty of σ(fNL) ~ 0.8 from the power spectrum alone and σ(fNL) ~ 0.2 when also including the bispectrum. However, challenges remain in applying photometric redshift indicators and understanding contributions to the squeezed bispectrum at higher orders.
1) The document discusses which seismic attributes are most useful for quantitative seismic reservoir characterization. It analyzes attributes such as zero phase amplitude, relative impedance, and absolute impedance.
2) The conclusion is that an absolute impedance inversion provides the best attribute in theory but is difficult in practice. A relative impedance inversion, which is easier to generate, works nearly as well for characterization.
3) Key advantages of relative impedance over zero phase amplitude include relating to geology rather than just impedance contrasts, and allowing comparison between seismic datasets and well logs after appropriate scaling. However, relative impedance lacks low frequency content included in absolute impedance.
This document discusses static correction in seismic data processing. It covers:
1) Static correction removes the effects of surface elevation changes and weathering layers on seismic data.
2) Examples are given of how water depth variations can induce pull-down of reflectors, though this does not represent real geology.
3) A figure from a research paper shows a seismic section with associated velocity information, geology, and an approximate static corrections diagram.
This is for student of geophysics who want to know about basic of multi component seismic. For further detail or any query you can drop me mail, my mail id id bprasad461@gmail.com
This document summarizes experiments demonstrating synthetic aperture radar interferometry (InSAR) using the TerraSAR-X and TanDEM-X satellites under crossing orbits. The experiments showed that InSAR is feasible with crossing orbits if small squints are applied. Repeat-pass InSAR acquisitions under large crossing angles also produced coherent fringes, enabling 1, 5, and 6 day repeats. Time series analysis of the Ronne Ice Shelf in Antarctica exploited the rapidly varying baselines between acquisitions to study ice shelf velocity gradients and decorrelation effects.
This document summarizes a study that used wide-swath interferometric synthetic aperture radar (InSAR) time series to map large-scale ground deformation over the Danakil depression in the Afar region of Ethiopia between 2006 and 2009. The time series analysis revealed deformation signals consistent with magmatic intrusions and inflation/deflation of volcanic centers. Modeling of the deformation supported deep magma intrusion beneath the central segment and lateral magma propagation and chamber inflation beneath Dabbahu volcano in the northern segment. The study demonstrated the potential of wide-swath InSAR time series for mapping long-wavelength ground deformation over large areas.
This document summarizes a study examining the hypergiant star ρ Cassiopeiae. The researchers developed a model to explain ρ Cassiopeiae's variable mass loss rate, high microturbulent velocity, and Hα emission line profile using a stochastic field of shock waves in the star's atmosphere. Their model successfully reproduced the observed mass loss rate, microturbulent velocity, and aspects of the Hα profile using only one parameter - the maximum Mach number of shock waves in the atmosphere. The model indicates that thin, hot regions behind shock waves are responsible for the observed microturbulence and contribute to Hα emission.
MUSE sneaks a peek at extreme ram-pressure stripping events. I. A kinematic s...Sérgio Sacani
- MUSE observations of the galaxy ESO137-001 reveal an extended gaseous tail over 30 kpc long traced by H-alpha emission, providing evidence of an extreme ram pressure stripping event as the galaxy falls into the massive Norma galaxy cluster.
- Analysis of the H-alpha kinematics and stellar velocity field show that ram pressure has removed the interstellar medium from the outer disk while the primary tail is still fed by gas from the galaxy center, with gravitational interactions not appearing to be the main mechanism of gas removal.
- The stripped gas retains evidence of the disk's rotational velocity out to around 20 kpc downstream, indicating the galaxy is moving radially along the plane of the sky, while
This document describes observations of the galaxy ESO137-001 using the MUSE instrument on the VLT. The key points are:
1) MUSE observations reveal an extended gas tail stretching over 30 kpc from the galaxy, tracing ongoing ram pressure stripping as it falls into the Norma galaxy cluster.
2) Analysis of the gas kinematics and stellar velocity field show that ram pressure has removed the interstellar medium from the outer disk while the primary tail is still fed by gas from the galaxy center.
3) The stripped gas retains evidence of the disk's rotational velocity out to 20 kpc downstream, indicating the galaxy is moving radially through the cluster. Beyond this the gas shows greater turbulence,
ALMA Observations of the Extraordinary Carina Pillars: A Complementary SampleSérgio Sacani
We present a study of six dusty and gaseous pillars (containing the HH 1004 and HH 1010 objects)
and globules (that contain the HH 666, HH 900, HH 1006, and HH 1066 objects) localized in the Carina
nebula using sensitive and high angular resolution (∼0.3′′) Atacama Large Millimeter/Sub-millimeter
Array (ALMA) observations. This is a more extensive study that the one presented in Cortes-Rangel
et al. (2020). As in this former study, we also analyzed the 1.3 mm continuum emission and C18O(2−1),
N2D+(3−2) and 12CO(2−1) spectral lines. These new observations revealed the molecular outflows
emanating from the pillars, the dusty envelopes+disks that are exciting them, and the extended HH
objects far from their respective pillars. We reveal that the masses of the disks+envelopes are in a
range of 0.02 to 0.38 M⊙, and those for the molecular outflows are of the order of 10−3 M⊙, which
suggests that their exciting sources might be low- or intermediate-mass protostars as already revealed
in recent studies at infrared and submillimeter bands. In the regions associated with the objects HH
900 and HH 1004, we report multiple millimeter continuum sources, from where several molecular
outflows emanate.
This document describes a technique for measuring interdiffusion in metallic multilayers during rapid heating using in situ X-ray reflectivity measurements. Key points:
- X-ray reflectivity is a sensitive probe for measuring interdiffusion as it is affected by changes in the composition modulation of the multilayer over time.
- A curved sample approach is used to collect a full reflectivity pattern simultaneously over a range of angles using a position-sensitive detector, allowing for in situ measurements during heating.
- Initial interdiffusion rates are determined from the decay of reflectivity peak intensities with increasing temperature. The activation energy for interdiffusion is found to be consistent with a grain boundary diffusion mechanism.
- At
Mapping the Skies of Ultracool Worlds: Detecting Storms and Spots with Extrem...Sérgio Sacani
Extremely large telescopes (ELTs) present an unparalleled opportunity to study the magnetism,
atmospheric dynamics, and chemistry of very low mass stars (VLMs), brown dwarfs, and exoplanets.
Instruments such as the Giant Magellan Telescope - Consortium Large Earth Finder (GMT/GCLEF),
the Thirty Meter Telescope’s Multi-Objective Diffraction-limited High-Resolution Infrared Spectrograph
(TMT/MODHIS), and the European Southern Observatory’s Mid-Infrared ELT Imager and Spectrograph (ELT/METIS) provide the spectral resolution and signal-to-noise (S/N) necessary to Doppler
image ultracool targets’surfaces based on temporal spectral variations due to surface inhomogeneities.
Using our publicly-available code, Imber, developed and validated in Plummer & Wang (2022), we
evaluate these instruments’abilities to discern magnetic star spots and cloud systems on a VLM star
(TRAPPIST-1); two L/T transition ultracool dwarfs (VHS J1256−1257 b and SIMP J0136+0933); and
three exoplanets (Beta Pic b and HR 8799 d and e). We find that TMT/MODHIS and ELT/METIS are
suitable for Doppler imaging the ultracool dwarfs and Beta Pic b over a single rotation. Uncertainties
for longitude and radius are typically . 10◦
, and latitude uncertainties range from ∼ 10◦
to 30◦
.
TRAPPIST-1’s edge-on inclination and low υ sin i provide a challenge for all three instruments while
GMT/GCLEF and the HR 8799 planets may require observations over multiple rotations. We compare
the spectroscopic technique, photometry-only inference, and the combination of the two. We find
combining spectroscopic and photometric observations can lead to improved Bayesian inference of
surface inhomogeneities and offers insight into whether ultracool atmospheres are dominated by spotted
or banded features.
This document summarizes the results of a sub-mm survey of the Carina Nebula complex conducted with the LABOCA instrument on the APEX telescope. The survey mapped an area of 1.25° × 1.25° at 870 μm, revealing the morphology and distribution of cold dust clouds with masses down to a few solar masses. The total mass of clouds detected is estimated to be around 60,000 M☉. The cloud morphologies range from large clouds of several thousand solar masses to small diffuse clouds of only a few solar masses. The distribution of sub-mm emission generally agrees with Spitzer 8 μm maps, identifying clouds interacting with massive stars as well as infrared dark clouds. The survey provides crucial
The document analyzes Spitzer Infrared Spectrograph (IRS) observations of warm molecular hydrogen (H2) gas in M51. It finds that the six H2 lines observed have distinct emission distributions across the galaxy. Lower J lines like H2 S(0) peak in the spiral arms, while higher J lines like H2 S(3) peak at the nucleus. The observations are used to model the H2 excitation temperature and mass in a warm (100-300 K) and hot (400-1000 K) phase. The warm gas peaks at 11 M_sun/pc^2 in the spiral arms, while the hot gas peaks at 0.24 M_sun/pc^2 at the
Atmospheric flows are governed by the equations of fluid dynamics. These equations are nonlinear. But because atmospheric flows are inhomogeneous and anisotropic, the nonlinearity may manifest itself only weakly through interactions of non-trivial mean flows with disturbances or eddies. In such situations, the quasi-linear (QL) approximation, that retains eddy-mean flow interactions but neglect eddy-eddy interactions, hold promise in resolving large-scale atmospheric dynamics. The statistics of the QL system corresponds to closing the hierarchy of statistical moments at the second order.
Hence, exploring QL dynamics paves the way for the development of direct statistical simulations of geophysical flows.
Using a hierarchy of idealized general circulation models, we identify when the QL approximation captures large-scale dynamics. We show that the QL dynamics fails to capture the flow when the dissipation of large-scale eddies occurs through strongly nonlinear eddy-eddy interactions in upper tropospheric surf zones, as it is often the case on Earth. But we demonstrate that the QL approximation captures eddy absorption when it arises from the shearing by the mean flow, for example when the eddy amplitude is small enough or the planetary rotation rate is large enough.
These results illustrate different classes of nonlinear processes that can control wave dissipation in the upper troposphere and show that in some parameter regimes the QL approximation is accurate to resolve large-scale dynamics.
Dust in the_polar_region_as_a_major_contributor_to_the_infrared_emission_of_a...Sérgio Sacani
The mid-infrared emission of the active galactic nucleus NGC 3783 was observed using interferometry over multiple epochs, providing dense coverage of position angles and baselines. The emission was found to be strongly elongated along a position angle of -52 degrees, closely aligned with the polar axis orientation of -45 degrees. The half-light radii were measured to be 20.0 mas by 6.7 mas, corresponding to an axis ratio of 3:1. This implies that 60-90% of the 8-13 micron emission is from the polar-elongated component. The observations support a scenario where the majority of mid-infrared emission in Seyfert galaxies originates from a dusty wind in the polar region,
Cyprus 2011 complexity extreme bursts and volatility bunching in solar terres...Nick Watkins
Nick Watkins presented research on complexity and volatility clustering in solar-terrestrial physics. The research began 15 years ago studying multiscale complexity in Earth's magnetosphere. Watkins' focus has been on self-similar and multifractal time series models. He highlighted work on temporal scaling of bursts above thresholds and volatility clustering, a multifractal feature also seen in some financial time series. Watkins advocated using the Kesten stochastic process as a "null" model for framing hypotheses about volatility bunching. The relevance extends beyond solar-terrestrial physics to complex systems modeling.
Modellistica Lagrangiana in ISAC Torino - risultati e nuovi sviluppiARIANET
The MicroSwift-Spray modelling system has been validated against experimental test cases from wind tunnel and field trials, showing it can reliably simulate particle dispersion. The MILORD long-range dispersion model was revived and applied to simulate the Fukushima nuclear accident and identify the source of CO2 peaks observed at a high-altitude Italian site, with results comparable to other models. Reviving MILORD demonstrated its ability to simulate long-range and regional-scale dispersion, including backwards trajectories, using less computation than some other models.
Airborne and underground matter-wave interferometers: geodesy, navigation and...Philippe Bouyer
The remarkable success of atom coherent manipulation techniques has motivated competitive research and development in precision metrology. Matter-wave inertial sensors – accelerometers, gyrometers, gravimeters – based on these techniques are all at the forefront of their respective measurement classes. Atom inertial sensors provide nowadays about the best accelerometers and gravimeters and allow, for instance, to make the most precise monitoring of gravity or to device precise tests of the weak equivalence principle (WEP). I present here some recent advances in these fields
X-RAY MEASUREMENTS OF THE PARTICLE ACCELERATION PROPERTIES AT INWARD SHOCKS I...Sérgio Sacani
We present new evidence that the bright non-thermal X-ray emission features in the interior of the Cassiopeia A
supernova remnant (SNR) are caused by inward moving shocks based on Chandra and NuSTAR observations. Several
bright inward-moving filaments were identified using monitoring data taken by Chandra in 2000–2014. These inwardmoving shock locations are nearly coincident with hard X-ray (15–40 keV) hot spots seen by NuSTAR. From proper
motion measurements, the transverse velocities were estimated to be in the range ∼2,100–3,800 km s−1
for a distance of
3.4 kpc. The shock velocities in the frame of the expanding ejecta reach values of ∼5,100–8,700 km s−1
, slightly higher
than the typical speed of the forward shock. Additionally, we find flux variations (both increasing and decreasing) on
timescales of a few years in some of the inward-moving shock filaments. The rapid variability timescales are consistent
with an amplified magnetic field of B ∼ 0.5–1 mG. The high speed and low photon cut-off energy of the inward-moving
shocks are shown to imply a particle diffusion coefficient that departs from the Bohm regime (k0 = D0/D0,Bohm ∼ 3–8)
for the few simple physical configurations we consider in this study. The maximum electron energy at these shocks is
estimated to be ∼8–11 TeV, smaller than the values of ∼15–34 TeV inferred for the forward shock. Cassiopeia A is
dynamically too young for its reverse shock to appear to be moving inward in the observer frame. We propose instead
that the inward-moving shocks are a consequence of the forward shock encountering a density jump of & 5–8 in the
surrounding material.
Discovery of rotational modulations in the planetary mass companion 2m1207b i...Sérgio Sacani
Rotational modulations of brown dwarfs have recently provided powerful constraints on the properties
of ultra-cool atmospheres, including longitudinal and vertical cloud structures and cloud evolution.
Furthermore, periodic light curves directly probe the rotational periods of ultra-cool objects. We
present here, for the first time, time-resolved high-precision photometric measurements of a planetarymass
companion, 2M1207b. We observed the binary system with HST/WFC3 in two bands and with
two spacecraft roll angles. Using point spread function-based photometry, we reach a nearly photonnoise
limited accuracy for both the primary and the secondary. While the primary is consistent with
a flat light curve, the secondary shows modulations that are clearly detected in the combined light
curve as well as in di↵erent subsets of the data. The amplitudes are 1.36% in the F125W and 0.78%
in the F160W filters, respectively. By fitting sine waves to the light curves, we find a consistent period
of 10.7+1.2
−0.6 hours and similar phases in both bands. The J- and H-band amplitude ratio of 2M1207b
is very similar to a field brown dwarf that has identical spectral type but di↵erent J-H color. Importantly,
our study also measures, for the first time, the rotation period for a directly imaged extra-solar
planetary-mass companion.
This document summarizes observations of the lensed galaxy HATLAS J142935.3-002836 (H1429-0028) from the Herschel-ATLAS survey. Optical spectroscopy revealed the foreground lens is at redshift 0.218, while the background galaxy is at redshift 1.027. High-resolution imaging from Hubble Space Telescope and Keck adaptive optics show the background galaxy is comprised of two components and a tidal tail, resembling a major merger. Analysis of ALMA observations of CO emission provides a dynamical mass estimate of one component as 5.8 ± 1.7 × 1010 M☉. Modeling of the spectral energy distribution indicates the total stellar mass is 1.32
First Observation of the Earth’s Permanent FreeOscillation s on Ocean Bottom ...Sérgio Sacani
The Earth’s hum is the permanent free oscillations of the Earth recorded in the absence ofearthquakes, at periods above 30 s. We present the first observations of its fundamental spheroidaleigenmodes on broadband ocean bottom seismometers (OBSs) in the Indian Ocean. At the ocean bottom,the effects of ocean infragravity waves (compliance) and seafloor currents (tilt) overshadow the hum. In ourexperiment, data are also affected by electronic glitches. We remove these signals from the seismic traceby subtracting average glitch signals; performing a linear regression; and using frequency-dependentresponse functions between pressure, horizontal, and vertical seismic components. This reduces the longperiod noise on the OBS to the level of a good land station. Finally, by windowing the autocorrelation toinclude only the direct arrival, the first and second orbits around the Earth, and by calculating its Fouriertransform, we clearly observe the eigenmodes at the ocean bottom.
Exocometary gas in_th_hd_181327_debris_ringSérgio Sacani
An increasing number of observations have shown that gaseous debris discs are not an
exception. However, until now we only knew of cases around A stars. Here we present the first
detection of 12CO (2-1) disc emission around an F star, HD 181327, obtained with ALMA
observations at 1.3 mm. The continuum and CO emission are resolved into an axisymmetric
disc with ring-like morphology. Using a Markov chain Monte Carlo method coupled with
radiative transfer calculations we study the dust and CO mass distribution. We find the dust is
distributed in a ring with a radius of 86:0 0:4 AU and a radial width of 23:2 1:0 AU. At
this frequency the ring radius is smaller than in the optical, revealing grain size segregation
expected due to radiation pressure. We also report on the detection of low level continuum
emission beyond the main ring out to 200 AU. We model the CO emission in the non-LTE
regime and we find that the CO is co-located with the dust, with a total CO gas mass ranging
between 1:2 10 6 M and 2:9 10 6 M, depending on the gas kinetic temperature and
collisional partners densities. The CO densities and location suggest a secondary origin, i.e.
released from icy planetesimals in the ring. We derive a CO cometary composition that is
consistent with Solar system comets. Due to the low gas densities it is unlikely that the gas is
shaping the dust distribution.
The Large APEX Bolometer Camera (LABOCA) is a new 295-bolometer submillimeter camera operating at 870 μm that has been commissioned for use on the 12 m Atacama Pathfinder Experiment (APEX) telescope. LABOCA offers unprecedented mapping capabilities for submillimeter continuum emission due to APEX's efficiency and the excellent atmospheric transmission at the site. LABOCA is designed to map large areas of the sky rapidly without the need for a chopping secondary mirror by using fast scanning techniques and correlating signals across the array to remove atmospheric contributions.
Similar to Solar prominence science with ALMA (20)
This document summarizes a presentation about solar prominences and tornadoes using data from multiple solar observatories. It discusses co-aligning different data sets to examine pixel-by-pixel correlations. Spectroscopy from Hinode/EIS provided a spectroscopic look at tornadoes. Doppler measurements showed motions within tornadoes. Images showed a tornado prominence eruption and subsequent coronal mass ejection. Upcoming Solar Orbiter and Parker Solar Probe missions were briefly described to get closer views of the Sun.
High-resolution observations of solar tornadoes and solar prominencesUniversity of Glasgow
Several observing campaigns have been carried out with the IRIS mission in coordination with other observatories to target solar prominences and prominence-like tornadoes. We focus here on observations between 2014 and 2016. The observational data is being complemented by a grid of non-LTE radiative transfer models producing synthetic Mg II line profiles. An algorithm is used to automatically extract relevant line profile parameters from the optically thick Mg II h and k lines, both on the observed and synthetic profiles. This allows us to study a large set of profiles and provide statistical results. We present our most recent findings from the combined analysis of synthetic spectra and of Mg II spectra acquired by IRIS, in terms of plasma parameters, magnetic fields, and dynamics, with the help of data from other observatories such as SDO, Hinode, the Meudon Solar Tower, and THEMIS. Implications for future high-resolution instruments are discussed.
This talk was given to Airdrie Astronomy Association on 22 March 2013. Some of the material was borrowed from Daniel Mueller (ESA) and the Solar Orbiter team. More information on Solar Orbiter can be found at http://sci.esa.int/solarorbiter
Solar spectroscopy is the study of the sun's spectrum of light. Important early developments included Newton observing the sun's spectrum using a prism in 1704, and Fraunhofer describing the dark absorption lines in 1817. Now high resolution spectroscopy is used to determine properties of the sun's atmosphere from the photosphere to the corona, and observe phenomena like solar flares. It provides insights into the sun's structure and energy transport mechanisms.
Plasma diagnostic in eruptive prominences from SDO/AIA observations at 304 ÅUniversity of Glasgow
The document discusses plasma diagnostic observations of eruptive solar prominences from SDO/AIA at 304 Angstroms. New non-LTE radiative transfer calculations allow plasma parameters like temperature, column mass, and radial velocity to vary, unlike previous models. The observations and new models show that the Helium II 304 Angstrom line intensity can either decrease or increase with increasing radial velocity, depending on changes in the plasma parameters. Allowing parameters to vary produces a range of intensities that matches the range seen in SDO/AIA observations qualitatively.
The document discusses modeling of helium line formation in solar prominences using radiative transfer modeling. It describes how the models account for the prominence-corona transition region and influence of radial plasma motions on line profiles and intensities. The modeling helps interpret observations from instruments like SOHO, Hinode, STEREO, and SDO to better understand the thermal structure and magnetic fields of prominences.
The document provides information about studying physics and astronomy at the University of Glasgow. It discusses Glasgow's location in Scotland, the university's colleges and schools, research areas and facilities in physics and astronomy, undergraduate and postgraduate degree programs, funding options, student life, and fees for international students. The university has a strong reputation for research and teaching in physics and astronomy.
We present SOPRA (Solar Off-limb Prominence Reconstruction Algorithm), an algorithm
which automatically detects prominences above the limb in EUV images taken in the He II
channel at 304 A and subsequently reconstructs the structures to extract their morphological parameters.
SOPRA determines the characteristics of radial intensity profiles outward from the limb and
uses Support Vector Machines in order to classify them as belonging to prominence or other
structures. Pixels detected as belonging to a prominence are then used as the starting point
to reconstruct the whole object by morphological image processing techniques.
The algorithm is applied to the entire SOHO/EIT data set and a catalogue of detected
prominences is produced. We present the initial statistical analysis of this catalogue, and
discuss its use for solar prominence research and for space weather monitoring.
We also assess the performance of SOPRA when applied to SDO/AIA images.
Solar radiation and plasma diagnostics outlines key concepts about solar radiation and how it is detected. It discusses (1) how solar radiation is formed through radiative transfer processes and depends on temperature, opacity, and optical depth; (2) the interaction of radiation with plasma is described by the radiative transfer equation; and (3) different spectral features form in different layers, with absorption lines seen in the photosphere and emission seen in the chromosphere.
Discovery of An Apparent Red, High-Velocity Type Ia Supernova at 𝐳 = 2.9 wi...Sérgio Sacani
We present the JWST discovery of SN 2023adsy, a transient object located in a host galaxy JADES-GS
+
53.13485
−
27.82088
with a host spectroscopic redshift of
2.903
±
0.007
. The transient was identified in deep James Webb Space Telescope (JWST)/NIRCam imaging from the JWST Advanced Deep Extragalactic Survey (JADES) program. Photometric and spectroscopic followup with NIRCam and NIRSpec, respectively, confirm the redshift and yield UV-NIR light-curve, NIR color, and spectroscopic information all consistent with a Type Ia classification. Despite its classification as a likely SN Ia, SN 2023adsy is both fairly red (
�
(
�
−
�
)
∼
0.9
) despite a host galaxy with low-extinction and has a high Ca II velocity (
19
,
000
±
2
,
000
km/s) compared to the general population of SNe Ia. While these characteristics are consistent with some Ca-rich SNe Ia, particularly SN 2016hnk, SN 2023adsy is intrinsically brighter than the low-
�
Ca-rich population. Although such an object is too red for any low-
�
cosmological sample, we apply a fiducial standardization approach to SN 2023adsy and find that the SN 2023adsy luminosity distance measurement is in excellent agreement (
≲
1
�
) with
Λ
CDM. Therefore unlike low-
�
Ca-rich SNe Ia, SN 2023adsy is standardizable and gives no indication that SN Ia standardized luminosities change significantly with redshift. A larger sample of distant SNe Ia is required to determine if SN Ia population characteristics at high-
�
truly diverge from their low-
�
counterparts, and to confirm that standardized luminosities nevertheless remain constant with redshift.
Mechanisms and Applications of Antiviral Neutralizing Antibodies - Creative B...Creative-Biolabs
Neutralizing antibodies, pivotal in immune defense, specifically bind and inhibit viral pathogens, thereby playing a crucial role in protecting against and mitigating infectious diseases. In this slide, we will introduce what antibodies and neutralizing antibodies are, the production and regulation of neutralizing antibodies, their mechanisms of action, classification and applications, as well as the challenges they face.
PPT on Direct Seeded Rice presented at the three-day 'Training and Validation Workshop on Modules of Climate Smart Agriculture (CSA) Technologies in South Asia' workshop on April 22, 2024.
Candidate young stellar objects in the S-cluster: Kinematic analysis of a sub...Sérgio Sacani
Context. The observation of several L-band emission sources in the S cluster has led to a rich discussion of their nature. However, a definitive answer to the classification of the dusty objects requires an explanation for the detection of compact Doppler-shifted Brγ emission. The ionized hydrogen in combination with the observation of mid-infrared L-band continuum emission suggests that most of these sources are embedded in a dusty envelope. These embedded sources are part of the S-cluster, and their relationship to the S-stars is still under debate. To date, the question of the origin of these two populations has been vague, although all explanations favor migration processes for the individual cluster members. Aims. This work revisits the S-cluster and its dusty members orbiting the supermassive black hole SgrA* on bound Keplerian orbits from a kinematic perspective. The aim is to explore the Keplerian parameters for patterns that might imply a nonrandom distribution of the sample. Additionally, various analytical aspects are considered to address the nature of the dusty sources. Methods. Based on the photometric analysis, we estimated the individual H−K and K−L colors for the source sample and compared the results to known cluster members. The classification revealed a noticeable contrast between the S-stars and the dusty sources. To fit the flux-density distribution, we utilized the radiative transfer code HYPERION and implemented a young stellar object Class I model. We obtained the position angle from the Keplerian fit results; additionally, we analyzed the distribution of the inclinations and the longitudes of the ascending node. Results. The colors of the dusty sources suggest a stellar nature consistent with the spectral energy distribution in the near and midinfrared domains. Furthermore, the evaporation timescales of dusty and gaseous clumps in the vicinity of SgrA* are much shorter ( 2yr) than the epochs covered by the observations (≈15yr). In addition to the strong evidence for the stellar classification of the D-sources, we also find a clear disk-like pattern following the arrangements of S-stars proposed in the literature. Furthermore, we find a global intrinsic inclination for all dusty sources of 60 ± 20◦, implying a common formation process. Conclusions. The pattern of the dusty sources manifested in the distribution of the position angles, inclinations, and longitudes of the ascending node strongly suggests two different scenarios: the main-sequence stars and the dusty stellar S-cluster sources share a common formation history or migrated with a similar formation channel in the vicinity of SgrA*. Alternatively, the gravitational influence of SgrA* in combination with a massive perturber, such as a putative intermediate mass black hole in the IRS 13 cluster, forces the dusty objects and S-stars to follow a particular orbital arrangement. Key words. stars: black holes– stars: formation– Galaxy: center– galaxies: star formation
PPT on Alternate Wetting and Drying presented at the three-day 'Training and Validation Workshop on Modules of Climate Smart Agriculture (CSA) Technologies in South Asia' workshop on April 22, 2024.
The cost of acquiring information by natural selectionCarl Bergstrom
This is a short talk that I gave at the Banff International Research Station workshop on Modeling and Theory in Population Biology. The idea is to try to understand how the burden of natural selection relates to the amount of information that selection puts into the genome.
It's based on the first part of this research paper:
The cost of information acquisition by natural selection
Ryan Seamus McGee, Olivia Kosterlitz, Artem Kaznatcheev, Benjamin Kerr, Carl T. Bergstrom
bioRxiv 2022.07.02.498577; doi: https://doi.org/10.1101/2022.07.02.498577
JAMES WEBB STUDY THE MASSIVE BLACK HOLE SEEDSSérgio Sacani
The pathway(s) to seeding the massive black holes (MBHs) that exist at the heart of galaxies in the present and distant Universe remains an unsolved problem. Here we categorise, describe and quantitatively discuss the formation pathways of both light and heavy seeds. We emphasise that the most recent computational models suggest that rather than a bimodal-like mass spectrum between light and heavy seeds with light at one end and heavy at the other that instead a continuum exists. Light seeds being more ubiquitous and the heavier seeds becoming less and less abundant due the rarer environmental conditions required for their formation. We therefore examine the different mechanisms that give rise to different seed mass spectrums. We show how and why the mechanisms that produce the heaviest seeds are also among the rarest events in the Universe and are hence extremely unlikely to be the seeds for the vast majority of the MBH population. We quantify, within the limits of the current large uncertainties in the seeding processes, the expected number densities of the seed mass spectrum. We argue that light seeds must be at least 103 to 105 times more numerous than heavy seeds to explain the MBH population as a whole. Based on our current understanding of the seed population this makes heavy seeds (Mseed > 103 M⊙) a significantly more likely pathway given that heavy seeds have an abundance pattern than is close to and likely in excess of 10−4 compared to light seeds. Finally, we examine the current state-of-the-art in numerical calculations and recent observations and plot a path forward for near-future advances in both domains.
Signatures of wave erosion in Titan’s coastsSérgio Sacani
The shorelines of Titan’s hydrocarbon seas trace flooded erosional landforms such as river valleys; however, it isunclear whether coastal erosion has subsequently altered these shorelines. Spacecraft observations and theo-retical models suggest that wind may cause waves to form on Titan’s seas, potentially driving coastal erosion,but the observational evidence of waves is indirect, and the processes affecting shoreline evolution on Titanremain unknown. No widely accepted framework exists for using shoreline morphology to quantitatively dis-cern coastal erosion mechanisms, even on Earth, where the dominant mechanisms are known. We combinelandscape evolution models with measurements of shoreline shape on Earth to characterize how differentcoastal erosion mechanisms affect shoreline morphology. Applying this framework to Titan, we find that theshorelines of Titan’s seas are most consistent with flooded landscapes that subsequently have been eroded bywaves, rather than a uniform erosional process or no coastal erosion, particularly if wave growth saturates atfetch lengths of tens of kilometers.
Sexuality - Issues, Attitude and Behaviour - Applied Social Psychology - Psyc...PsychoTech Services
A proprietary approach developed by bringing together the best of learning theories from Psychology, design principles from the world of visualization, and pedagogical methods from over a decade of training experience, that enables you to: Learn better, faster!
Mending Clothing to Support Sustainable Fashion_CIMaR 2024.pdfSelcen Ozturkcan
Ozturkcan, S., Berndt, A., & Angelakis, A. (2024). Mending clothing to support sustainable fashion. Presented at the 31st Annual Conference by the Consortium for International Marketing Research (CIMaR), 10-13 Jun 2024, University of Gävle, Sweden.
Farming systems analysis: what have we learnt?.pptx
Solar prominence science with ALMA
1. N. Labrosse, P. Antolin, J.L. Ballester, R. Brajsa,
S. Gunár, B. Schmieder, M. Temmer, S. Wedemeyer
Solar prominence
science with ALMA
2. Prominence studies with ALMA – Nicolas Labrosse
ALMA / IRIS / DKIST Workshop – 2016/03/15
Key points
ALMA can help to answer important open questions about prominences and filaments
What is their thermal structure?
What is their spatial fine-structure?
Can we constrain the magnetic field structure?
ALMA will
- provide precise temperature estimates at high cadence
- benefit from the support from other instruments (Hα, HMI, ...)
3. Prominence studies with ALMA – Nicolas Labrosse
ALMA / IRIS / DKIST Workshop – 2016/03/15
Prominence 101
Above figure from Mackay et al (2010)
See also Labrosse et al (2010), Parenti (2014), Vial & Engvold (2015)
Range of scales
Respond to heating
processes
Magnetic field
Eruptions, flares, CMEs
Cool, dense plasma at
chromospheric temperatures
4. Prominence studies with ALMA – Nicolas Labrosse
ALMA / IRIS / DKIST Workshop – 2016/03/15
Some questions to be addressed by ALMA
The thermal structure of solar prominences at millimetre wavelengths
What is the fine-scale thermal structure of solar prominences and filaments at high
spatial resolution in their main body and in the prominence-corona transition region?
How does the prominence plasma react to various heating processes?
How is the dynamics of the plasma related on small scales and on large scales to the
structure in temperature of solar prominences?
The spatial structure of solar prominences at millimetre wavelengths
How is the fine-scale structure of prominences shaped by the magnetic field?
How do Active Region and Quiet Sun prominences differ in millimetre wavelengths?
- height dependence of thermal emission
- wave power versus period
- flow magnitudes
- timescale / range of temperature changes
- onset of prominence activation
- distribution and sizes of the fine structures
- dynamics and temporal evolution of the fine
structures
- filling factor, corresponding to the fraction
occupied by the fine structures
Observables provided by ALMA
5. Prominence studies with ALMA – Nicolas Labrosse
ALMA / IRIS / DKIST Workshop – 2016/03/15
Powerful combination: ALMA, SDO, Hα observations (e.g.,
Kanzelhöhe, Paris-Meudon)
How is the fine-scale structure of filaments
shaped and what is their role in erupting
filaments?
Observational study by Su et al.
(2014) and simulations by
Wedemeyer-Böhm et al. (2012)
showed magnetized “tornado”
structures at the basis of
filament formation. Those
structures are assumed to play a
role in the eruption of a
filament.
ALMA high-resolution data of
such fine structures will enable
us to thoroughly study their
physical characteristics (mass
flows, oscillations, relations to
magnetic field) and association
to mass eruptions.
6. Prominence studies with ALMA – Nicolas Labrosse
ALMA / IRIS / DKIST Workshop – 2016/03/15
Enhancement
of density at the
edges
Tornado
Prominence
( Parenti)
Corona
Plasma structure of prominence legs
Levens et al 2015
7. Prominence studies with ALMA – Nicolas Labrosse
ALMA / IRIS / DKIST Workshop – 2016/03/15
(Schmieder et al 2015, Levens et al 2016)
The magnetic field is between 25 - 60 G
The inclination is 90 degrees:
horizontal field
Magnetic field
structure and
orientation
8. 8
• Ubiquitous transverse MHD waves
• Heating: Fading in cool line (104 K),
subsequent appearance in hot line (105 K)
• Out-of-phase POS motion & LOS velocity
• Thread-like structure
Hinode/SOT(Ca II, 10,000 K)
IRIS/SJI (Si IV, 100,000)
Hinode/SOT(JAXA/NAOJ)IRIS(NASA)
200 s
x-t diagram
104 K
105 K
IRIS/Hinode observations
Motion of prominence plasma crossing the slit
Time [sec]
Dopplervelocityfrom
IRIS[km/s]
Displacement[km]
1,000
500
0
-1,000
-500
0 100 200 300 400
10
5
0
-10
-5
(Okamoto+2015,
Antolin+2015)
9. Numerical model Prominence thread
Hinode field-
of-view
Sun
Alfvénicwave
magnetic field
lines
Prominence
9
11. Small-scale
vortices
45° LOS plane
Si IV (~ 105 K)
Mg II k Doppler velocity
Heating of
chromospheric
plasma
Observational
signatures
Mg II k Line width
Line
broadening
Displacement
2000kmDistance
Time 200 s
Mg II k (~ 104 K)
slit
Prominence
thread
1
Observable with ALMA
✔︎
✔︎
thread-like
structure
Turbulent
spectrum
✔︎
(Antolin+2015,
Okamoto+2015)
12. Prominence studies with ALMA – Nicolas Labrosse
ALMA / IRIS / DKIST Workshop – 2016/03/15
Background temperature fluctuations
effect on propagation of slow MHD waves
Ballester et al, A&A, accepted
13. Prominence studies with ALMA – Nicolas Labrosse
ALMA / IRIS / DKIST Workshop – 2016/03/15
Temperature fluctuations
14. Prominence studies with ALMA – Nicolas Labrosse
ALMA / IRIS / DKIST Workshop – 2016/03/15
Filaments on the disc
1.0 - quiet Sun level
Brajša et al., 2007, Sol.Pys. 245, 167
Brajša et al., 2009, AA 493, 613
Metsähovi
λ = 8 mm
27 May 1993
HTRs, Tb > TQSL
LTRs, Tb < TQSL
15. Prominence studies with ALMA – Nicolas Labrosse
ALMA / IRIS / DKIST Workshop – 2016/03/15
Filaments on the disc
From Phillips et al (2015)
16. Prominence studies with ALMA – Nicolas Labrosse
ALMA / IRIS / DKIST Workshop – 2016/03/15
What will ALMA see?
For prominence plasma, radiation at ALMA wavelengths has its origins in free-free
continuum emission
LTE can be assumed, so source function is Planck function
Radio wavelengths: Rayleigh-Jeans approximation
Hence brightness temperature is
We take the absorption coefficient as in Dulk (1995) and get for
See Wedemeyer et al (2015), Heinzel et al (2015)
NB: All population densities may depart from their LTE values
17. Prominence studies with ALMA – Nicolas Labrosse
ALMA / IRIS / DKIST Workshop – 2016/03/15
Prominence Fine Structures
Heinzel et al (2015)
18. Prominence studies with ALMA – Nicolas Labrosse
ALMA / IRIS / DKIST Workshop – 2016/03/15
Brightness temp. maps of fine structures
Visualization of the 3D Whole-
Prominence Fine Structure (WPFS)
model developed by Gunár & Mackay
(2015a,b) viewed from the side as a
prominence above the solar limb.
The resolution of the displayed
synthetic images is 150 km.
Gunár et al. (2016 – in prep)
Hα line centre
0.45 mm
3 mm
9 mm
19. Prominence studies with ALMA – Nicolas Labrosse
ALMA / IRIS / DKIST Workshop – 2016/03/15
2D cylindrical models
Gouttebroze & Labrosse (2009)
Labrosse & Rodger (2016)
Figure courtesy A. Rodger
20. Prominence studies with ALMA – Nicolas Labrosse
ALMA / IRIS / DKIST Workshop – 2016/03/15
1D prominence model Labrosse & Gouttebroze (2004)
surface
centre
Anzer & Heinzel (1999)
21. Prominence studies with ALMA – Nicolas Labrosse
ALMA / IRIS / DKIST Workshop – 2016/03/15
1D prominence model: brightness temp.
Loukitcheva et al (2004)
22. Prominence studies with ALMA – Nicolas Labrosse
ALMA / IRIS / DKIST Workshop – 2016/03/15
1D contribution functions
12292 K
Plasma optically thick for λ>2.2mm
⇒ observing in bands 3 and 6 is key (Cycle 4)
23. Prominence studies with ALMA – Nicolas Labrosse
ALMA / IRIS / DKIST Workshop – 2016/03/15
Suggested observing sequence for ALMA
Only band 3 (84 - 116 GHz, 3.6-2.6mm) and band 6 (211 - 275 GHz, 1.4-1.1mm) will be
available. Hence, depending on scientific objective:
Large mosaic, with 150 pointings, at low cadence, in two bands – suitable for large-
scale studies of thermal structure and spatial structure
Small mosaic, with <40 pointings, at moderate cadence – suitable for small-scale
studies of dynamical changes in thermal structure and spatial structure (incl.
“tornadoes”)
High-cadence, single point sit-and-stare, with ~2s per map, only one band – suitable for
oscillation studies
Support from other GBOs (e.g. Hα, D3, Ca II) and from space valuable
Complementary data, probing different layers
IHOP campaigns, 1 or 2 weeks long, particularly useful for prominences
See Wedemeyer et al. (2015,2016)
24. Prominence studies with ALMA – Nicolas Labrosse
ALMA / IRIS / DKIST Workshop – 2016/03/15
Key points
ALMA can help to answer important open questions about prominences and filaments
What is their thermal structure?
What is their spatial fine-structure?
Can we constrain the magnetic field structure?
Challenges
When observing at the limb: side lobes of PSF could swamp out off-limb signal with
large contributions from solar disk
Calibration and continuous observing
Small field-of-view of ALMA requires mosaicking, implying lower cadence
ALMA will
- provide precise temperature estimates at high cadence
- benefit from the support from other instruments (Hα, HMI, ...)