The document discusses how climate change is intensifying the global water cycle. It notes that glaciers and alpine glaciers are melting, temperatures and sea levels are rising, and precipitation patterns are changing. There is evidence that heavy precipitation events have increased in the US, resulting in more frequent and severe flooding in some areas. Climate models project continued changes, such as further increases in heavy precipitation and drought in some regions, but uncertainties remain regarding regional predictions. Satellite observations are providing valuable new insights into global water patterns.
Noah, Joseph, And High-Resolution PaleoclimatologyScott St. George
In 1968, Benoit Mandelbrot and James Wallis published an article titled ‘Noah, Joseph, and operational Hydrology’ in the journal Water Resources Research. In it, they argued that hydrological models of the day were not able to estimate the true risk of extreme floods or prolonged drought, and that rare hydrological events were much more common than usually assumed.
In this lecture, I’ll review how high-resolution paleoenvironmental archives can help us judge more accurately the risks posed by the ‘Noah’- and ‘Joseph’-style events described by Mandelbrot and Wallis. I’ll give particular emphasis to the environmental information recovered from the rings of ancient trees, and explain how dendrochronology (tree-ring research) has been used to redefine the ‘flood of record’, test potential avenues for long-lead climate predictions, and gage the performance of state-of-the-art climate models.
Many of the decisions we make about environmental issues are based on experience. Whether we're setting limits for the use of scarce resources, estimating the risks posed by natural hazards, or deciding how to manage protected areas, our plans for the future often reflect our understanding of the past. The problem is that, when it comes to the environment, our society has a fairly short memory. In this presentation, Dr. St. George will discuss how the study of ancient trees is expanding our perspective on the natural history of the northern Plains and helping to answer questions about what the future may hold for Minnesota's environment.
Don’t call it a comeback: Studying ancient floods to prepare for future hazardsScott St. George
How long do we need to watch a river before its behavior holds no more surprises? In this country, instrumental measurements of river stage and discharge stretch back a century or more, but this observed history still provides only a rough guide to the risks of future extreme floods. In this lecture, I’ll outline how paleoflood hydrology expands our perspective on river history by combining historical, botanical, and geological evidence of earlier (and ofttimes unknown) floods. And I’ll explain how we can interpret those physical clues left behind by ancient floods to improve hazard assessments for at-risk communities, support decisions about flood infrastructure, and investigate the long-term effects of climate or land-use changes on flooding. Because what has happened before can happen again, most everyone near a river would profit by keeping a longer memory of old floods.
A B S T R A C T
Urban stormwater lakes in cold regions are ice-covered for substantial parts of the winter. It has long been considered that the ice-covered period is the “dormant season,” during which ecological processes are inactive. However, little is known about this period due to the historical focus on the open-water season. Recent pioneering research on ice-covered natural lakes has suggested that some critical ecological processes play out on the ice. The objective of this study was to investigate the active processes in ice-covered stormwater lakes. Data collected during a two-year field measurement program at a stormwater lake located in Edmonton, Alberta, Canada were analyzed. The lake was covered by ice from November to mid-April of the following year. The mean value of chlorophyll-a during the ice-covered period was 22.09% of the mean value for the open-water season, suggesting that primary productivity under ice can be important. Nitrogen and phosphorus were remarkably higher during the ice-covered period, while dissolved organic carbon showed little seasonal variation. Under ice-covered conditions, the total phosphorus was the major nutrient controlling the ratio of total nitrogen to total phosphorus, and a significant positive correlation existed between total phosphorus and chlorophyll-a when the ratio was smaller than 10. The results provide preliminary evidence of the critical nutrient processes in the Stormwater Lake during the ice-covered period.
Expecting the unexpected: The relevance of old floods to modern hydrologyScott St. George
As one of the most destructive hazards on our planet, floods kill thousands of people and cause billions of dollars in property damage every year. We usually try to gage the risk of future floods by fitting mathematic functions to hydrological data and then extrapolating the upper tail of those distributions. But because large floods are rare and river gage records are short, the conventional approach can sometimes drastically underestimate the threat posed to communities and infrastructure by extreme floods. In this lecture, I’ll argue that paleoflood hydrology — the study of ancient floods as recorded by river and lake sediments, trees, caves, and historical documents — is absolutely essential to judge the real risk of large, rare floods. And I’ll use examples from North America to illustrate how a ‘deeper river memory’ can help people evaluate their own vulnerability to floods, weigh the potential benefits of proposed infrastructure projects, and become more aware of what nature is truly capable of producing.
Every year, trees in temperate and boreal forests go through a cycle of dormancy and activity that produces a new layer of tracheids, fibers and other woody cells around their stem. The end result of this process - a tree ring - is one of the most obvious signs in nature documenting the passage of time and the character of that year’s weather. Measurements of tree-ring widths are the most widely-distributed and best replicated source of surrogate environmental information on the planet and are one of the main archives used to estimate changes in regional and global climate during the past several centuries or millennia.
In this lecture, I describe the structure and characteristics of the Northern Hemisphere tree-ring width network, and outline how these data are linked with key aspects of local climate and the global climate system. More generally, by describing the characteristics of the Northern Hemisphere tree-ring width network and the diversity of its relations with varying aspects of the global climate system, this presentation highlights the breadth and quality of environmental information that may be recovered from the width of annual growth layers in temperate and boreal trees.
The "Year Without A Summer" was not a year without a ringScott St. George
The Tambora eruption of 1815 cooled the planet and caused the "Year Without A Summer" in western Europe and eastern North America. But was it cold enough to cause trees across the Northern Hemisphere to skip a ring?
Noah, Joseph, And High-Resolution PaleoclimatologyScott St. George
In 1968, Benoit Mandelbrot and James Wallis published an article titled ‘Noah, Joseph, and operational Hydrology’ in the journal Water Resources Research. In it, they argued that hydrological models of the day were not able to estimate the true risk of extreme floods or prolonged drought, and that rare hydrological events were much more common than usually assumed.
In this lecture, I’ll review how high-resolution paleoenvironmental archives can help us judge more accurately the risks posed by the ‘Noah’- and ‘Joseph’-style events described by Mandelbrot and Wallis. I’ll give particular emphasis to the environmental information recovered from the rings of ancient trees, and explain how dendrochronology (tree-ring research) has been used to redefine the ‘flood of record’, test potential avenues for long-lead climate predictions, and gage the performance of state-of-the-art climate models.
Many of the decisions we make about environmental issues are based on experience. Whether we're setting limits for the use of scarce resources, estimating the risks posed by natural hazards, or deciding how to manage protected areas, our plans for the future often reflect our understanding of the past. The problem is that, when it comes to the environment, our society has a fairly short memory. In this presentation, Dr. St. George will discuss how the study of ancient trees is expanding our perspective on the natural history of the northern Plains and helping to answer questions about what the future may hold for Minnesota's environment.
Don’t call it a comeback: Studying ancient floods to prepare for future hazardsScott St. George
How long do we need to watch a river before its behavior holds no more surprises? In this country, instrumental measurements of river stage and discharge stretch back a century or more, but this observed history still provides only a rough guide to the risks of future extreme floods. In this lecture, I’ll outline how paleoflood hydrology expands our perspective on river history by combining historical, botanical, and geological evidence of earlier (and ofttimes unknown) floods. And I’ll explain how we can interpret those physical clues left behind by ancient floods to improve hazard assessments for at-risk communities, support decisions about flood infrastructure, and investigate the long-term effects of climate or land-use changes on flooding. Because what has happened before can happen again, most everyone near a river would profit by keeping a longer memory of old floods.
A B S T R A C T
Urban stormwater lakes in cold regions are ice-covered for substantial parts of the winter. It has long been considered that the ice-covered period is the “dormant season,” during which ecological processes are inactive. However, little is known about this period due to the historical focus on the open-water season. Recent pioneering research on ice-covered natural lakes has suggested that some critical ecological processes play out on the ice. The objective of this study was to investigate the active processes in ice-covered stormwater lakes. Data collected during a two-year field measurement program at a stormwater lake located in Edmonton, Alberta, Canada were analyzed. The lake was covered by ice from November to mid-April of the following year. The mean value of chlorophyll-a during the ice-covered period was 22.09% of the mean value for the open-water season, suggesting that primary productivity under ice can be important. Nitrogen and phosphorus were remarkably higher during the ice-covered period, while dissolved organic carbon showed little seasonal variation. Under ice-covered conditions, the total phosphorus was the major nutrient controlling the ratio of total nitrogen to total phosphorus, and a significant positive correlation existed between total phosphorus and chlorophyll-a when the ratio was smaller than 10. The results provide preliminary evidence of the critical nutrient processes in the Stormwater Lake during the ice-covered period.
Expecting the unexpected: The relevance of old floods to modern hydrologyScott St. George
As one of the most destructive hazards on our planet, floods kill thousands of people and cause billions of dollars in property damage every year. We usually try to gage the risk of future floods by fitting mathematic functions to hydrological data and then extrapolating the upper tail of those distributions. But because large floods are rare and river gage records are short, the conventional approach can sometimes drastically underestimate the threat posed to communities and infrastructure by extreme floods. In this lecture, I’ll argue that paleoflood hydrology — the study of ancient floods as recorded by river and lake sediments, trees, caves, and historical documents — is absolutely essential to judge the real risk of large, rare floods. And I’ll use examples from North America to illustrate how a ‘deeper river memory’ can help people evaluate their own vulnerability to floods, weigh the potential benefits of proposed infrastructure projects, and become more aware of what nature is truly capable of producing.
Every year, trees in temperate and boreal forests go through a cycle of dormancy and activity that produces a new layer of tracheids, fibers and other woody cells around their stem. The end result of this process - a tree ring - is one of the most obvious signs in nature documenting the passage of time and the character of that year’s weather. Measurements of tree-ring widths are the most widely-distributed and best replicated source of surrogate environmental information on the planet and are one of the main archives used to estimate changes in regional and global climate during the past several centuries or millennia.
In this lecture, I describe the structure and characteristics of the Northern Hemisphere tree-ring width network, and outline how these data are linked with key aspects of local climate and the global climate system. More generally, by describing the characteristics of the Northern Hemisphere tree-ring width network and the diversity of its relations with varying aspects of the global climate system, this presentation highlights the breadth and quality of environmental information that may be recovered from the width of annual growth layers in temperate and boreal trees.
The "Year Without A Summer" was not a year without a ringScott St. George
The Tambora eruption of 1815 cooled the planet and caused the "Year Without A Summer" in western Europe and eastern North America. But was it cold enough to cause trees across the Northern Hemisphere to skip a ring?
Large-scale dendrochronology and low-frequency climate variabilityScott St. George
Large-scale low-frequency variability has emerged as a priority for climate research, but instrumental observations are not long enough to characterize this behavior or gage its impacts on dependent geophysical or ecological systems. As the leading source of high-resolution paleoclimate information in the middle- and high-latitudes, tree rings are essential to understand low-frequency variability prior to the instrumental period. But even though tree rings possess several advantages as climate proxies, like other natural archives they also have their own particular impediments. In this lecture, Dr. St. George will describe the structure and characteristics of the Northern Hemisphere tree-ring width network, and outline how the fingerprint of decadal and multidecadal climate variability encoded within ancient trees varies across the hemisphere.
Flood rings: Paleoflood evidence in tree-ring anatomyScott St. George
In low-gradient, low energy rivers, forms of tree-ring evidence such as impact scars or stem deformation do not provide useful evidence of past floods. In this talk, I explain the strengths and limitations of wood anatomy as tools in in paleoflood hydrology.
The decadal character of northern California's winter precipitationScott St. George
Starting in the 1930s, northern California has experienced major decade-to-decade swings in the amount of precipitation that falls during winter. Is this behavior
Expanding the window - the past, present, and future of Minnesota's waterScott St. George
Nearly all decisions about water in Minnesota relate either directly or indirectly to data collected by the state’s hydrological observing network. Because most gauges were installed in early 20th century, as a whole the network provides us with roughly a 100-year ‘window’ to estimate flood risks, develop worst-case scenarios for drought, and set maximum allowable withdrawals for aquifers. But when we rely exclusively on observations made during this relatively brief interval, we may inadvertently increase our exposure to hydrological ‘surprises’. In order to make sound decisions about water in Minnesota, we need to expand this window: into the past, drawing upon historical accounts and natural archives; and into the future, via projections from climate and hydrological models. By cultivating a broader perspective on hydrological variability and extremes across the state, we will be better prepared to ensure adequate water supplies and mitigate the impacts of future floods and droughts.
In many settings, trees growing on floodplains provide an important source of indirect evidence that may be used to infer the occurrence, extent, and magnitude of floods prior to direct observations. That evidence may take several forms, including external scars caused by abrasion or impact from floating debris, anatomical changes within the annual growth increment following prolonged stem or root inundation, or tilting or uprooting due to the hydraulic pressure of floodwaters. Likely the most useful characteristic of paleoflood studies based on floodplain trees is their relatively high temporal resolution and dating accuracy compared to most other methods. Dendrochronological methods can routinely date past floods to the year of their occurrence and, in rare cases, can estimate the timing of floods that occur during the growing season to within two weeks. This high degree of chronological control, which is surpassed only by that provided by direct observation or instrumentation, can be used to determine whether floods in separate watersheds were synchronous or offset by several years and test hypotheses that suppose linkages between extreme floods and specific forcing mechanisms. Furthermore, the wide geographic distribution of tree species with dateable rings combined with the broad suite of methods available to examine interconnections between floods and tree growth allow this style of paleoflood hydrology to be applied to many settings that are not suitable for techniques that depend on geological evidence. Future paleoflood research involving tree rings will need to strike a balance between improving our understanding of the biological and fluvial processes that link tree growth to past events, and providing answers to questions about flood dynamics and hazards that are needed to safeguard people and property from future floods.
Lower than expected air temperatures and sunshine are now both increasing; rivers are generally running high. Willapa Bay unfolds its beauty from a bird’s-eye view. The spring phytoplankton bloom is picking up in Puget Sound. A large red-orange-brown bloom persists in southern Hood Canal at a scale sufficient for the MODIS satellite to pick up. Jellyfish are still going strong in southern inlets. Ocean climate indices (PDO, NPGO and Upwelling Index) explain much of the variability in Puget Sound temperature, salt and oxygen. Nutrients, however, are steadily increasing while sub-surface algal pigments (chlorophyll a) are declining!
From our climate panel in Grand Junction on August 4:
Our Forest, Our Water, Our Land: Local Impacts on Climate Change. Sponsored by Conservation Colorado, Mesa County Library, Math & Science Center
EOPS_April_6_2016,
Despite warmer air temperatures, normal snowpack in the mountains suggest that summer freshwater flows into Puget Sound might be higher than last year. As of April, the spring plankton bloom has extended across Central and South Puget Sound. Ferry data shows chlorophyll increasing after March 25 and expanding across the area. With water temperatures above normal as a carry-over from 2015, jellyfish patches are numerous in inlets of South Sound and in Sinclair Inlet, unusual for this time of year. Check out the tiny burrowing ostracods as well as our Washington Conservation Corps Intern analyzing seawater oxygen.
Ecology Publication No. 16-03-072
Abi area in Nigeria borders the salinity enriched
Lower Benue Trough (LBT) and plans are currently
underway to extend large-scale irrigation facilities under
construction in the LBT to Abi area. In order to generate
baseline soil and water salinity information about Abi area
under non-irrigation condition, integrated information from
constrained analyses of vertical electrical sounding data,
two-dimensional electrical resistivity tomographies and
laboratory analyses of soil and water samples were used to
assess and map the spatial salinity distribution. Existence
of widespread heterogeneities in the distribution of soil and
water salinity between the shaly and sandy materials that
dominate the shallow geology of the area was observed.
Minimum values of water electrical conductivity (WEC)
and total dissolved solids (TDS) were observed to be 19.2
lS/cm and 13 mg/L, respectively, in the sandstone-dominated
areas. Maximum values of WEC and TDS were
observed to be 931.0 lS/cm and 624 mg/L, respectively,
within the shale-dominated areas. Soil electrical conductivity
was observed to vary from 5.0 lS/cm in the sandstone
areas to 14.0 lS/cm in the shale-dominated areas.
Minimum and maximum soil pH observations were 4.53 in
the shale-dominated area and 6.55 in the sandstone-dominated
area, respectively. These results show that the water
and soil resources in the area vary from fresh to slightly
saline and non-saline to high salinity levels, respectively.
Consequently, both resources are still good for agricultural
purposes.
Factors affecting monsoon precipitation in NepalSagar Parajuli
I did a brief study about the factors affecting monsoon precipitation in Nepal few months ago for a class project. I am sharing the slides as it is relevant to the recent flooding in north India and Nepal.
Large-scale dendrochronology and low-frequency climate variabilityScott St. George
Large-scale low-frequency variability has emerged as a priority for climate research, but instrumental observations are not long enough to characterize this behavior or gage its impacts on dependent geophysical or ecological systems. As the leading source of high-resolution paleoclimate information in the middle- and high-latitudes, tree rings are essential to understand low-frequency variability prior to the instrumental period. But even though tree rings possess several advantages as climate proxies, like other natural archives they also have their own particular impediments. In this lecture, Dr. St. George will describe the structure and characteristics of the Northern Hemisphere tree-ring width network, and outline how the fingerprint of decadal and multidecadal climate variability encoded within ancient trees varies across the hemisphere.
Flood rings: Paleoflood evidence in tree-ring anatomyScott St. George
In low-gradient, low energy rivers, forms of tree-ring evidence such as impact scars or stem deformation do not provide useful evidence of past floods. In this talk, I explain the strengths and limitations of wood anatomy as tools in in paleoflood hydrology.
The decadal character of northern California's winter precipitationScott St. George
Starting in the 1930s, northern California has experienced major decade-to-decade swings in the amount of precipitation that falls during winter. Is this behavior
Expanding the window - the past, present, and future of Minnesota's waterScott St. George
Nearly all decisions about water in Minnesota relate either directly or indirectly to data collected by the state’s hydrological observing network. Because most gauges were installed in early 20th century, as a whole the network provides us with roughly a 100-year ‘window’ to estimate flood risks, develop worst-case scenarios for drought, and set maximum allowable withdrawals for aquifers. But when we rely exclusively on observations made during this relatively brief interval, we may inadvertently increase our exposure to hydrological ‘surprises’. In order to make sound decisions about water in Minnesota, we need to expand this window: into the past, drawing upon historical accounts and natural archives; and into the future, via projections from climate and hydrological models. By cultivating a broader perspective on hydrological variability and extremes across the state, we will be better prepared to ensure adequate water supplies and mitigate the impacts of future floods and droughts.
In many settings, trees growing on floodplains provide an important source of indirect evidence that may be used to infer the occurrence, extent, and magnitude of floods prior to direct observations. That evidence may take several forms, including external scars caused by abrasion or impact from floating debris, anatomical changes within the annual growth increment following prolonged stem or root inundation, or tilting or uprooting due to the hydraulic pressure of floodwaters. Likely the most useful characteristic of paleoflood studies based on floodplain trees is their relatively high temporal resolution and dating accuracy compared to most other methods. Dendrochronological methods can routinely date past floods to the year of their occurrence and, in rare cases, can estimate the timing of floods that occur during the growing season to within two weeks. This high degree of chronological control, which is surpassed only by that provided by direct observation or instrumentation, can be used to determine whether floods in separate watersheds were synchronous or offset by several years and test hypotheses that suppose linkages between extreme floods and specific forcing mechanisms. Furthermore, the wide geographic distribution of tree species with dateable rings combined with the broad suite of methods available to examine interconnections between floods and tree growth allow this style of paleoflood hydrology to be applied to many settings that are not suitable for techniques that depend on geological evidence. Future paleoflood research involving tree rings will need to strike a balance between improving our understanding of the biological and fluvial processes that link tree growth to past events, and providing answers to questions about flood dynamics and hazards that are needed to safeguard people and property from future floods.
Lower than expected air temperatures and sunshine are now both increasing; rivers are generally running high. Willapa Bay unfolds its beauty from a bird’s-eye view. The spring phytoplankton bloom is picking up in Puget Sound. A large red-orange-brown bloom persists in southern Hood Canal at a scale sufficient for the MODIS satellite to pick up. Jellyfish are still going strong in southern inlets. Ocean climate indices (PDO, NPGO and Upwelling Index) explain much of the variability in Puget Sound temperature, salt and oxygen. Nutrients, however, are steadily increasing while sub-surface algal pigments (chlorophyll a) are declining!
From our climate panel in Grand Junction on August 4:
Our Forest, Our Water, Our Land: Local Impacts on Climate Change. Sponsored by Conservation Colorado, Mesa County Library, Math & Science Center
EOPS_April_6_2016,
Despite warmer air temperatures, normal snowpack in the mountains suggest that summer freshwater flows into Puget Sound might be higher than last year. As of April, the spring plankton bloom has extended across Central and South Puget Sound. Ferry data shows chlorophyll increasing after March 25 and expanding across the area. With water temperatures above normal as a carry-over from 2015, jellyfish patches are numerous in inlets of South Sound and in Sinclair Inlet, unusual for this time of year. Check out the tiny burrowing ostracods as well as our Washington Conservation Corps Intern analyzing seawater oxygen.
Ecology Publication No. 16-03-072
Abi area in Nigeria borders the salinity enriched
Lower Benue Trough (LBT) and plans are currently
underway to extend large-scale irrigation facilities under
construction in the LBT to Abi area. In order to generate
baseline soil and water salinity information about Abi area
under non-irrigation condition, integrated information from
constrained analyses of vertical electrical sounding data,
two-dimensional electrical resistivity tomographies and
laboratory analyses of soil and water samples were used to
assess and map the spatial salinity distribution. Existence
of widespread heterogeneities in the distribution of soil and
water salinity between the shaly and sandy materials that
dominate the shallow geology of the area was observed.
Minimum values of water electrical conductivity (WEC)
and total dissolved solids (TDS) were observed to be 19.2
lS/cm and 13 mg/L, respectively, in the sandstone-dominated
areas. Maximum values of WEC and TDS were
observed to be 931.0 lS/cm and 624 mg/L, respectively,
within the shale-dominated areas. Soil electrical conductivity
was observed to vary from 5.0 lS/cm in the sandstone
areas to 14.0 lS/cm in the shale-dominated areas.
Minimum and maximum soil pH observations were 4.53 in
the shale-dominated area and 6.55 in the sandstone-dominated
area, respectively. These results show that the water
and soil resources in the area vary from fresh to slightly
saline and non-saline to high salinity levels, respectively.
Consequently, both resources are still good for agricultural
purposes.
Factors affecting monsoon precipitation in NepalSagar Parajuli
I did a brief study about the factors affecting monsoon precipitation in Nepal few months ago for a class project. I am sharing the slides as it is relevant to the recent flooding in north India and Nepal.
Weather!: Meteorology and Meteorological Collections at the Royal Irish Acade...The Royal Irish Academy
Weather!: Meteorology and Meteorological Collections at the Royal Irish Academy and Met Éireann - Mairéad Treanor, Librarian, Met Éireann. For additional information including audio recordings to accompany this presentation please click here - http://www.ria.ie/library/exhibitions/lunchtime-lecture-series.aspx.
Disclaimer:
The Royal Irish Academy has prepared the content of this website responsibly and carefully, but disclaims all warranties, express or implied, as to the accuracy of the information contained in any of the materials. The views expressed are the authors’ own and not those of the Royal Irish Academy.
Hydroclimatology of Sariz Creek Watershed, Located In Seyhan Basin, And Simulation Of The Snowmelt Runoff Using Remote Sensing And Geographic Information Systems (Mountain Watershed Case Study). Presented by Ibrahim Gürer at the "Perth II: Global Change and the World's Mountains" conference in Perth, Scotland in September 2010.
Climate Change Basics: Issues and Impacts for BoatingNASBLA
State Climatologist David Zierden presented Climate Change Basics: Issues and Impacts for Boating to the National Association of State Boating Law Administrators on September 9, 2008
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
The year 2014 tied with 2010 as the warmest year on record for the last century. The melting of Greenland, mountain glaciers, and thermal expansion is raising sea levels four times faster than in 1900. Sea level rises of 2 to 6 feet are predicted by the end of the century. Flood highs from hurricanes Sandy and Katrina were ~ 10 feet.
The article “Treading Water” in the February 2015 "National Geographic" tells how Dutch Docklands LLC sees profit not loss from rising sea levels. They are building floating homes in Miami, FL. A floating classroom could assure ASPEC’s long-term future. It would provide a place to meet in the event of flooding by the 10-foot ocean surges that accompany hurricanes.
Dr. Carr describes how increasing greenhouse gases, mostly carbon dioxide from the burning of fossil fuels, trap the radiation that is warming our planet. Advances in non-carbon emitting energy sources can reduce global warming. Solar PV panels are now generating electricity at $0.07/kWhr, less than the national utility average of $0.12kWhr. Rising sea levels are a better measure of global warming than atmospheric temperature, as 90% of our planet’s heat content is in our oceans.
You can learn more at www.RiskyBusiness.org.
Dr. Jay Famiglietti - 21st Century Water Security and Implications for Animal...John Blue
21st Century Water Security and Implications for Animal Agriculture - Dr. Jay Famiglietti, Associate Professor at University of California, Irvine and Senior Water Scientist at the NASA Jet Propulsion Laboratory, from the 2015 NIAA Annual Conference titled 'Water and the Future of Animal Agriculture', March 23 - March 26, 2015, Indianapolis, IN, USA.
More presentations at http://www.trufflemedia.com/agmedia/conference/2015_niaa_water_future_animal_ag
EOPS_August_24_2016,
In July, conditions were normalizing, yet river flows remained lower, continuing into August. July also saw lower oxygen appearing in southern Puget Sound. By August, jellyfish are occurring in high numbers in Eld and Budd Inlet. South Puget Sound has Noctiluca drifting at the surface in large orange lines in many places and red-brown blooms widespread in finger inlets, as well as in Sinclair Inlet. Central Sound surface-water temperatures are high, still in the 60s, and algae are abundant. See what we are measuring to understand ocean acidification in Puget Sound.
Publication No. 16-03-076
1. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Ensuring Water in a Changing WorldEnsuring WorldAssociation of State and Territorial Health Officials (ASTHO) webinar series on the human health effects of climate change. April 29th, 2008Climate Change & The Global Water Cycle: Recent Regional Experiences Soroosh Sorooshian Center for Hydrometeorology and Remote SensingUniversity of California Irvine
2. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
University of California Irvine (UCI) and Arizona (UA)
3. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
and many more …
CHRS & Affiliates: A truly International Team
4. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
A Unique Planet: Blue, Green and alive!
5. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Earth's atmosphere: 78% nitrogen, 21% oxygen, and 1% other gasesAtmosphere of Earth vs. Mars and Venus
7. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Distribution of Fresh Water Use90.833.4% 17.1% 49.5% 4607.0% 6.0% 87.0% 36.4718.6% 22.0% 59.4% 11760.0% 17.0% 23.0% 467.3445.2% 13.1% 41.7% 3804.0%3.0% 93.0%AgricultureIndustryDomesticFresh Water Use(109Cubic Meters)
Water Source
Water UseUSAChinaIndiaRussia
Japan
Brazil92% 6% 2% 70.3Iran
8. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Increasing Population: Number of Mega Cities
Global Urban population 1970: ~37%
2010: ~53% Projected Global Population: 8.3 Billion by 2025
9. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
The Big Question as to Whether Our Planet Is Warming Up and The Hydrologic Cycle is Intensifying, has been addressed by The Recent IPCC Report
10. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Evidence for reality of climate change: Glaciers MeltingEvidence Melting19092000Muir Glacier, Alaska1900 2003Alpine glacier, Austria1900 AustriaToboggan Glacier Alaska
Provided By: Kevin Trenberth
11. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Source: NASA GISS 2007
Global Temperature Anomalies: 2007Tied (with 1998) for the second warmest year (2005 Warmest)
12. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Global Warming And Hydrologic Cycle ConnectionHeatingTemperatureEvaporationWater Holding CapacityAtmospheric Moisture
Source: Gi-Hyeon Park Green House EffectConsequence: Intensification of Hydrologic cycle
13. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Observed changes: Heavy Precipitation
ƒFrom 1908-2002:
ƒTotal annual precipitation across the contiguous U.S. increased 7%
ƒHeavy daily Precipitation events have increased by 20%
ƒRainfall associated with warmer climates are more due to extreme events compared to colder climates Facts from Observations100Confidence Index
Source: Tom Karl NCDC-NOAA 2007
14. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Record Floods: Among the worst Natural Disasters
15. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Record Floods: Among the worst Natural Disasters
17. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
0200400600800100012001400Jun-48Jun-52Jun-56Jun-60Jun-64Jun-68Jun-72Jun-76Jun-80Jun-84Jun-88Jun-92Jun-96Jun-00 Event total precipitation (mm) Event duration (days) 246081012020040060080010001200Total precipitation (mm)and duration (days)of extreme events in Texas Normal annual precipitation inTexas is 650~750mmSource: J. Nielsen-Gammon et al., 2005Extreme Precipitation events: Texas, USA (1948-2001)
18. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
American River Runoff Annual Maximum 1-Day Flow 02550751001251501752002252501900190519101915192019251930193519401945195019551960196519701975198019851990199520002005Water Year 1,000 cfs Unimpaired Runoff at Fair Oaks Changes in Peak FlowsAmerican River, California
Red Line = Construction of Folsom DamFrom: J. Andrew DWR-DFM
19. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Observed changes: Drought Reconstruction
•Within the past millennium there have been severe droughts in both the western U.S. and Midwest that have lasted for multiple decades (50 years). Drought as documented in the paleoclimaticrecord? 1005Confidence IndexSource: Tom Karl NCDC-NOAA 2007
20. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
16th century “megadrought” 1930’s dustbowl>100 year “megadroughts”
2000-year Climate history of central U.S. DustBowl2000 yrs. agoTodayThe US Breadbasket: The Mid-West
Source: Overpeck2004
21. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Ensuring Water in a Changing WorldEnsuring WorldChallenge of predicting the future Climate: While we Attempt to Improve Our Scientific Understanding of the Climate System, We Face Major Issues With Uncertainties in Information We Can Provide to “Users” Challenge
22. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Some Results at the Seasonal to Inter-annual and Longer time Scales:
Climate Predictions into the Future!
23. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Climate model Predictions about the future? Æglobally
DJF Precipitation Changes
CM2 -Old model
CM3 -Updated model
Significant differences
in regional outcomes! Source: Hadley Center (Climate Change Projections)
24. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Model annual precipitation trends over 21stcentury Hadley Center: Southwest dries outWhat to tell water managers? Canadian Center: Southwest extremely wetSource: US National Assessment Report, 2000
What do climate models tell us about the future?
25. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Canadian Prairie drought 1999-2005500 km2001/02Source: Ronald Stewart
26. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
SEASONAL PREDICTIONS: Summer of 2005 -Canada
PREDICTION
OBSERVATIONAboveNormalBelowNormal
Source: Ronald Stewart
27. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
(flooding at the end of the drought) St. Jean de Baptiste, ManitobaJuly 2005Source: Ronald Stewart
28. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Recent Extreme Conditions in the U.S. Southwest
Lake Powell, Colorado River, USANormal YearsSever Multi-year Drought through 2004
Source: J. Kane SRP 2004
29. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Eye-Catching Article in Science Magazine
30. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Observed changes: Drought
•U.S. droughts show
pronounced multi-year
to multi-decadal
variability, but no
convincing evidence
for long-term trends
toward more or
fewer events. Drought activity during the 20thand early 21stCentury1005Confidence Index
Based on Palmer Drought Index
Moderate to Extreme Drought
Source: Tom Karl NCDC-NOAA 2007
31. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Practices in Factoring in Climate and Extreme Events in Water Resources: Engineering Approach: Control, Store, Use & Deliver for Multi-Purposes
32. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Hoover DamGlen Canyon DamCentral Arizona Project Aqueduct
A Century of Water Resources Development: Engineering success!
33. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Time of Construction = 1935
Total Storage Capacity = 38.6 BCM
Annual Inflow = 15.4 BCM
Drainage Area = 432,500 Km2
Time to fill =2.5 Years
Power Generation = 2,074 MW
Time of Construction = 1963
Total Storage Capacity = 33.3 BCM
Annual Inflow = 15.4 BCM
Drainage Area = 280,570 Km2
Time to fill = 2.24 Years
Power Generation = 1,356 MWHoover DamGlen Canyon Dam
Built-In Resiliency in water resources Systems!
34. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Colorado Basin400% California Region100% Storage Capacity/Streamflow Relationship B. Imam, CHRS-UC Irvine
35. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
“News From Space” Satellite ObservationsSatellite Observations
36. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
SatelliteHuman Eye Reflectance( % ) Visible Range804000.4 0.6 0.8 1.0 1.2 1.4 1.6 1.8 2.0 2.2 2.4 2.6 Wavelength (μm) 40200Bare SoilHealthyVegetation40200StressedVegetation40200FreshSnowSeaWater 543210 0 2 4 6 8 10 12 14 16
Remote Sensing Systems (Spectral Signal)
37. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Current Meteorological and Earth Observing Satellites in Space
38. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Precipitation Observations: Which to trust??
Sources: R. Fulton, D.-J. Seo. and J. Breidenbach, AMS Short-Course on QPE/QPF, 2002
39. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Satellite Products: Promising future
40. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
A Key Requirement! Measurement of Rainfall is a Major Challenge
41. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Temporal Scale Importance:Daily Precip. at 2 stations020401611162126020401611162126Frequency 6.7% Intensity 37.5 mmFrequency 67% Intensity 3.75 mmMonthlyAmount 75 mmAmount 75 mmlocalfloodssoil moisture replenishedvirtually no runoffABSource: K. Trenberth, NCARSource: NCAR
44. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Satellite Products: Promising future
45. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Satellite Products: Promising future
46. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Global Flood Archive for 2007http://www.dartmouth.edu/~floods/
47. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
U.S. Drought Monitor ( Multi Agency Effort)
48. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
U.S. Drought Outlook ( Multi Agency Effort)
49. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
AHPS Flood Forecast system (U.S.A)
50. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Monitoring of Global Fires from Space
51. Center for Hydrometeorology and Remote Sensing, University of California, Irvine
Thank You For ListeningThank ListeningThe Rio Grande River, NM Photo: J. Sorooshian 2005