This document contains information from Douglas P. Boyle of the Nevada State Climate Office regarding water year precipitation and snowpack conditions across Nevada. Maps show that much of Nevada is experiencing below average precipitation and snowpack, with percentages of normal ranging from 1% to 83% across different regions as of April 16, 2015. The document also includes information on reservoir status, drought conditions according to the U.S. Drought Monitor, seasonal forecasts and other climate data and resources available through the Nevada State Climate Office.
Responding to Climate Change: Impacts, Uncertainty and Adaptation - lecture 1...Jose M. Molina
Presentation by Jose Molina, Course 500.111 - Fall 2015 Johns Hopkins University: Global Climate Phenomena & Climate Change. Reflections on California Drought, Water Supply in Western US, Massive Fires in Indonesia, and Precipitation changes in the Tropics
Monitoring Climate Variability and Impact in NV: What's A PA Country Gal Doin...DRIscience
How did a PA Country Gal become a science geek and end up in the desert?
What is the Desert Research Institute?
Some of my research projects include Monitoring Climate Variability, Impact of Climate on Basin Scale ET, and hot new NV research
Danielle Shannon (Michigan Technological University and NIACS), presented at the Adapting Forested Watersheds to Climate Change Workshop, at The Waters, Minocqua, WI on March 15-16, 2017. The workshop was hosted by the Northern Institute of Applied Climate Science (NIACS), USDA Climate Hubs, and the Wisconsin Initiative on Climate Change Impacts (WICCI).
Details at www.forestadaptation.org/water
Dennis Todey (of USDA ARS and USDA Midwest Climate Hub), presented at the Adapting Forested Watersheds to Climate Change Workshop, at The Waters, Minocqua, WI on March 15-16, 2017. The workshop was hosted by the Northern Institute of Applied Climate Science (NIACS), USDA Climate Hubs, and the Wisconsin Initiative on Climate Change Impacts (WICCI).
Stephen Handler (Forest Service, and NIACS), presented at the Adapting Forested Watersheds to Climate Change Workshop, at The Waters, Minocqua, WI on March 15-16, 2017. The workshop was hosted by the Northern Institute of Applied Climate Science (NIACS), USDA Climate Hubs, and the Wisconsin Initiative on Climate Change Impacts (WICCI).
Responding to Climate Change: Impacts, Uncertainty and Adaptation - lecture 1...Jose M. Molina
Presentation by Jose Molina, Course 500.111 - Fall 2015 Johns Hopkins University: Global Climate Phenomena & Climate Change. Reflections on California Drought, Water Supply in Western US, Massive Fires in Indonesia, and Precipitation changes in the Tropics
Monitoring Climate Variability and Impact in NV: What's A PA Country Gal Doin...DRIscience
How did a PA Country Gal become a science geek and end up in the desert?
What is the Desert Research Institute?
Some of my research projects include Monitoring Climate Variability, Impact of Climate on Basin Scale ET, and hot new NV research
Danielle Shannon (Michigan Technological University and NIACS), presented at the Adapting Forested Watersheds to Climate Change Workshop, at The Waters, Minocqua, WI on March 15-16, 2017. The workshop was hosted by the Northern Institute of Applied Climate Science (NIACS), USDA Climate Hubs, and the Wisconsin Initiative on Climate Change Impacts (WICCI).
Details at www.forestadaptation.org/water
Dennis Todey (of USDA ARS and USDA Midwest Climate Hub), presented at the Adapting Forested Watersheds to Climate Change Workshop, at The Waters, Minocqua, WI on March 15-16, 2017. The workshop was hosted by the Northern Institute of Applied Climate Science (NIACS), USDA Climate Hubs, and the Wisconsin Initiative on Climate Change Impacts (WICCI).
Stephen Handler (Forest Service, and NIACS), presented at the Adapting Forested Watersheds to Climate Change Workshop, at The Waters, Minocqua, WI on March 15-16, 2017. The workshop was hosted by the Northern Institute of Applied Climate Science (NIACS), USDA Climate Hubs, and the Wisconsin Initiative on Climate Change Impacts (WICCI).
EOPS_May_2_2016,
Spring air temperatures are higher - it has been sunny and dry. The snowpack is quickly disappearing as temperatures are up to 7 °F warmer at higher elevations. Snowmelt-fed rivers are running very high. How does this affect water quality in Puget Sound? A strong spring phytoplankton bloom extends across Puget Sound and the Strait of Juan de Fuca. Water temperatures are still higher than normal and jellyfish are already numerous in southern inlets. The high biological activity is causing organic material to drift at the surface and wash onto beaches. Do you know how fast a Sand Star can move?
Ecology Publication No. 16-03-073
Projected Climate Change Impacts for Rhode Island’s Coast: A Summary of the S...riseagrant
Learn the facts about climate change in Rhode Island, existing impacts, and near-term projections presented by Austin Becker, URI College of Environmental Life Sciences
EOPS_June_5_2017,
Cooler and wetter conditions early in 2017 have set the stage for a favorable supply of freshwater. River flows are all above normal due to melting of the abundant snowpack from warmer May air temperatures. This is creating significantly fresher conditions in Puget Sound surface waters. Algae blooms are limited to some yellow-green blooms growing in bays near the Kitsap Peninsula and blooms near estuaries of the Skagit, Stillaguamish, and Puyallup Rivers. Red blooms are present in rivers feeding into Willapa Bay. Also see what is “blooming” in the sediments of Puget Sound.
Ecology Publication No. 17-03-070
EOPS_July_20_2016,
Through June, air temperatures and sunlight were higher than normal. Recent rain generally improved river flows. However, the Fraser river flow remains extremely low, reducing water exchange with the ocean. Water temperatures are still breaking records, yet dissolved oxygen levels are normal. Coastal bays are influenced by upwelling and exhibit lower oxygen and higher salinities. Puget Sound algae are thriving with blooms observed in many South Sound inlets. Macro-algae is seen piling up on beaches and drifting in Central Sound. Jellyfish smacks are numerous in Eld and Budd Inlets. Our fliers notice seals hanging out at the beach!
Ecology Publication No. 16-03-075
Keith Nislow (Forest Service and Northeast Climate Science Center) presented at the Adapting Forested Watersheds to Climate Change Workshop, at Antioch University New England, Keene, NH on April 4-5, 2017. The workshop was hosted by the Northern Institute of Applied Climate Science (NIACS), USDA Climate Hubs, and Trout Unlimited.
Toxic effects of heavy metals : Lead and Arsenicsanjana502982
Heavy metals are naturally occuring metallic chemical elements that have relatively high density, and are toxic at even low concentrations. All toxic metals are termed as heavy metals irrespective of their atomic mass and density, eg. arsenic, lead, mercury, cadmium, thallium, chromium, etc.
Richard's aventures in two entangled wonderlandsRichard Gill
Since the loophole-free Bell experiments of 2020 and the Nobel prizes in physics of 2022, critics of Bell's work have retreated to the fortress of super-determinism. Now, super-determinism is a derogatory word - it just means "determinism". Palmer, Hance and Hossenfelder argue that quantum mechanics and determinism are not incompatible, using a sophisticated mathematical construction based on a subtle thinning of allowed states and measurements in quantum mechanics, such that what is left appears to make Bell's argument fail, without altering the empirical predictions of quantum mechanics. I think however that it is a smoke screen, and the slogan "lost in math" comes to my mind. I will discuss some other recent disproofs of Bell's theorem using the language of causality based on causal graphs. Causal thinking is also central to law and justice. I will mention surprising connections to my work on serial killer nurse cases, in particular the Dutch case of Lucia de Berk and the current UK case of Lucy Letby.
Professional air quality monitoring systems provide immediate, on-site data for analysis, compliance, and decision-making.
Monitor common gases, weather parameters, particulates.
What is greenhouse gasses and how many gasses are there to affect the Earth.moosaasad1975
What are greenhouse gasses how they affect the earth and its environment what is the future of the environment and earth how the weather and the climate effects.
Comparing Evolved Extractive Text Summary Scores of Bidirectional Encoder Rep...University of Maribor
Slides from:
11th International Conference on Electrical, Electronics and Computer Engineering (IcETRAN), Niš, 3-6 June 2024
Track: Artificial Intelligence
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DERIVATION OF MODIFIED BERNOULLI EQUATION WITH VISCOUS EFFECTS AND TERMINAL V...Wasswaderrick3
In this book, we use conservation of energy techniques on a fluid element to derive the Modified Bernoulli equation of flow with viscous or friction effects. We derive the general equation of flow/ velocity and then from this we derive the Pouiselle flow equation, the transition flow equation and the turbulent flow equation. In the situations where there are no viscous effects , the equation reduces to the Bernoulli equation. From experimental results, we are able to include other terms in the Bernoulli equation. We also look at cases where pressure gradients exist. We use the Modified Bernoulli equation to derive equations of flow rate for pipes of different cross sectional areas connected together. We also extend our techniques of energy conservation to a sphere falling in a viscous medium under the effect of gravity. We demonstrate Stokes equation of terminal velocity and turbulent flow equation. We look at a way of calculating the time taken for a body to fall in a viscous medium. We also look at the general equation of terminal velocity.
This presentation explores a brief idea about the structural and functional attributes of nucleotides, the structure and function of genetic materials along with the impact of UV rays and pH upon them.
Salas, V. (2024) "John of St. Thomas (Poinsot) on the Science of Sacred Theol...Studia Poinsotiana
I Introduction
II Subalternation and Theology
III Theology and Dogmatic Declarations
IV The Mixed Principles of Theology
V Virtual Revelation: The Unity of Theology
VI Theology as a Natural Science
VII Theology’s Certitude
VIII Conclusion
Notes
Bibliography
All the contents are fully attributable to the author, Doctor Victor Salas. Should you wish to get this text republished, get in touch with the author or the editorial committee of the Studia Poinsotiana. Insofar as possible, we will be happy to broker your contact.
Deep Behavioral Phenotyping in Systems Neuroscience for Functional Atlasing a...Ana Luísa Pinho
Functional Magnetic Resonance Imaging (fMRI) provides means to characterize brain activations in response to behavior. However, cognitive neuroscience has been limited to group-level effects referring to the performance of specific tasks. To obtain the functional profile of elementary cognitive mechanisms, the combination of brain responses to many tasks is required. Yet, to date, both structural atlases and parcellation-based activations do not fully account for cognitive function and still present several limitations. Further, they do not adapt overall to individual characteristics. In this talk, I will give an account of deep-behavioral phenotyping strategies, namely data-driven methods in large task-fMRI datasets, to optimize functional brain-data collection and improve inference of effects-of-interest related to mental processes. Key to this approach is the employment of fast multi-functional paradigms rich on features that can be well parametrized and, consequently, facilitate the creation of psycho-physiological constructs to be modelled with imaging data. Particular emphasis will be given to music stimuli when studying high-order cognitive mechanisms, due to their ecological nature and quality to enable complex behavior compounded by discrete entities. I will also discuss how deep-behavioral phenotyping and individualized models applied to neuroimaging data can better account for the subject-specific organization of domain-general cognitive systems in the human brain. Finally, the accumulation of functional brain signatures brings the possibility to clarify relationships among tasks and create a univocal link between brain systems and mental functions through: (1) the development of ontologies proposing an organization of cognitive processes; and (2) brain-network taxonomies describing functional specialization. To this end, tools to improve commensurability in cognitive science are necessary, such as public repositories, ontology-based platforms and automated meta-analysis tools. I will thus discuss some brain-atlasing resources currently under development, and their applicability in cognitive as well as clinical neuroscience.
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Nevada State Climate Office - Doug Bolye, Nevada State Climatologist, University of Nevada, Reno
1. Department of Geography, University of Nevada Reno Douglas P. Boyle
Nevada State Climate Office
Douglas P. Boyle
douglasb@unr.edu
Department of Geography
University of Nevada, Reno
3. Department of Geography, University of Nevada Reno Douglas P. Boyle
Precipitation % of Normal
Eastern
Nevada
Northern Great Basin
Lower
Humboldt
Southern Nevada
Walker
Carson
Owyhee River Snake
River
Clover
Valley
Upper
Humboldt
Truckee
Lake
Tahoe
51
78
69
68
83
48
48
83
52
77
53
Water Year (Oct 1)
to Date Precipitation
Basin-wide Percent
of 1981-2010 Average
unavailable *
<50%
50 - 69%
70 - 89%
90 - 109%
110 - 129%
130 - 149%
>= 150%
Prepared by:
USDA/NRCS National Water and Climate Center
Portland, Oregon
http://www.wcc.nrcs.usda.gov
Provisional data
subject to revision
Nevada/California SNOTEL Water Year (Oct 1) to Date Precipitation % of Normal
0 75 15037.5
Miles
* Data unavailable
at time of posting
or measurement
is not representative
at this time of year
The water year to date precipitation percent of normal represents the
accumulated precipitation found at selected SNOTEL sites in or near the basin
compared to the average value for those sites on this day. Data based on
the first reading of the day (typically 00:00).
Apr 16, 2015
4. Department of Geography, University of Nevada Reno Douglas P. Boyle
SWE % of Normal
Eastern
Nevada
Northern Great Basin
Lower
Humboldt
Southern Nevada
Walker
Carson
Owyhee River Snake
River
Clover
Valley
Upper
Humboldt
Truckee
Lake
Tahoe
16
27
26
6
1
17
24
37
15
58
0
Current Snow
Water Equivalent
Basin-wide Percent
of 1981-2010 Median
unavailable *
<50%
50 - 69%
70 - 89%
90 - 109%
110 - 129%
130 - 149%
>= 150%
Prepared by:
USDA/NRCS National Water and Climate Center
Portland, Oregon
http://www.wcc.nrcs.usda.gov
Provisional data
subject to revision
Nevada/California SNOTEL Current Snow Water Equivalent (SWE) % of Normal
0 70 14035
Miles
* Data unavailable
at time of posting
or measurement
is not representative
at this time of year
The current snow water equivalent percent of normal represents the
snow water equivalent found at selected SNOTEL sites in or near the basin
compared to the average value for those sites on this day. Data based on
the first reading of the day (typically 00:00).
Apr 16, 2015
13. Department of Geography, University of Nevada Reno Douglas P. Boyle
U.S.D.M – Policy Impacts
2015 S ecretarial D ro u g h t D es ign atio n s -A ll D ro u g h t
Alaska 1:58,102,399
Hawaii 1:19,740,053
S ecretarial D rou gh t D es ign ation s for 2015
Disaster Incidents as of April 15, 2015
State Boundary
County Boundary
Tribal Lands
USDA Farm Service Agency
Primary Counties: 302
Production, Emergencies and Compliance Division
Washington, D.C. Contiguous Counties: 150
1:23,520,203 Puerto Rico 1:5,592,808April 15, 2015
Accuracy of Drought Monitor is important!
14. Department of Geography, University of Nevada Reno Douglas P. Boyle
Assessing Drought Status
Questions from public about the DM
• Why is ____ D4?
• Why isn’t ____ D4?
• What does D4 mean?
• Is the drought over?
• How much precipitation do we need to end the drought?
• When will that happen?
• Is the drought due to global warming?
• Are we in the beginning (or middle) of a “mega-drought?
CA-NV DM & Water Conditions Discussion
• Discuss latest local water conditions, impacts, actions, and the DM
• Provide a coordinated response to DM authors and others
• Single most valuable resource for NSCO.
16. Department of Geography, University of Nevada Reno Douglas P. Boyle
Recommendations to DM Authors
Move to D4 Move to D3 Move to D1
“As of the end of
December, Denio was
above 150% of normal
precipitation while
eastward at
McDermitt it was
closer to 50%”
We need help!
17. Department of Geography, University of Nevada Reno Douglas P. Boyle
Availability of Information
Large number of weather &
climate products available
18. Department of Geography, University of Nevada Reno Douglas P. Boyle
L.T. Drought Indicator Blend
19. Department of Geography, University of Nevada Reno Douglas P. Boyle
S.T. Drought Indicator Blend
22. Department of Geography, University of Nevada Reno Douglas P. Boyle
Availability of Analysis Tools
23. Department of Geography, University of Nevada Reno Douglas P. Boyle
Availability of Observations
How accurate are these products
and tools?
The topography, geology, and
weather patterns in the West
require a large number of real
climate observations to characterize
the spatial and temporal variability.
We have the least number of
climate observations in these areas.
Desperately need more real
observations of climate variables to
understand and assess uncertainty
and product limitations.
We need your help!
24. Department of Geography, University of Nevada Reno Douglas P. Boyle
3-month Temperature Forecast
25. Department of Geography, University of Nevada Reno Douglas P. Boyle
3-month Precipitation Forecast
26. Department of Geography, University of Nevada Reno Douglas P. Boyle
Seasonal Drought Outlook
http://go.usa.gov/hHTe
U.S. Seasonal Drought Outlook
Author:
Rich Tinker
NOAA/NWS/NCEP/Climate Prediction Center
Drought Tendency During the Valid Period
Valid for April 16 - July 31, 2015
Released April 16, 2015
Depicts large-scale trends based
on subjectively derived probabilities
guided by short- and long-range
statistical and dynamical forecasts.
Use caution for applications that
can be affected by short lived events.
"Ongoing" drought areas are
based on the U.S. Drought Monitor
areas (intensities of D1 to D4).
NOTE: The tan areas imply at least
a 1-category improvement in the
Drought Monitor intensity levels by
the end of the period, although
drought will remain. The green
areas imply drought removal by the
end of the period (D0 or none).
Drought persists/intensifies
Drought remains but improves
Drought removal likely
Drought development likely