Showing posts with label WEATHER. Show all posts
Showing posts with label WEATHER. Show all posts

Wednesday, February 5, 2014

WATCHING EDNA, STUBBORN FLETCHER FROM SPACE

Right:  This infrared image of Tropical Storm Edna was taken by NOAA's polar orbiting satellite, NOAA-19 on Feb. 4 at 1443 UTC/9:43 a.m.
Image Credit: NRL/NOAA
FROM:  NASA 

NASA Satellite Catches Australia's Newborn Tropical Storm Edna and Stubborn Fletcher

Northeastern Australia has been watching two tropical low pressure areas over the last several days, and NASA's Aqua satellite captured both in one infrared image. Tropical Storm Edna developed on February 4, while Fletcher, known also as System 94P continued to have a medium chance for development.
On February 3 at 15:53 UTC/10:53 a.m. EST, NASA's Aqua satellite passed over Queensland, Australia and the AIRS or Atmospheric Infrared Sounder instrument captured infrared data on both storms. System 94P/Fletcher was in the Gulf of Carpentaria and over the Northwest region of
Queensland, while newborn Edna formed in the South Pacific Ocean east of Queensland.

Tropical Storm Edna Moving Toward New Caledonia

System 93P strengthened between February 3 and 4 into Tropical Depression 12P and then Tropical Storm Edna, northwest New Caledonia. By 1500 UTC/10 a.m. EST Edna was about 392 nautical miles northwest of New Caledonia, near 17.2 south latitude and 161.5 east longitude. Edna had maximum sustained winds near 35 knots/40 mph/62 kph. It was moving to the southeast at 19 knots/21.8 mph/35.1 kph.

NASA's AIRS data showed very cold cloud top temperatures in powerful thunderstorms within Edna that have the potential for heavy rainfall. Infrared data also showed that Edna's circulation has consolidated and convection has deepened/strengthened with bands of thunderstorms, mostly north of the center, were wrapping more tightly into the low-level center of circulation.
AIRS data also showed that sea surface temperatures were around 28C/82.4F, warm enough to contribute to strengthening the system. Sea surface temperatures need to be at least 26.6C/80F in order for a tropical cyclone to maintain intensity. Warmer temperatures than that can help in increased evaporation with the formation of thunderstorms that make up a tropical cyclone. However, as Edna continues tracking southward, the storm will run into cooler sea surface temperatures that will squelch any significant intensification.
Text credit:  Rob Gutro

NASA's Goddard Space Flight Center

Friday, January 17, 2014

PRESIDENT'S CLIMATE ACTION PLAN REVIEWED BY GSA

FROM:  GENERAL SERVICES ADMINISTRATION
President's Climate Action Plan R
Review of the President's Climate Action Plan
Senate Committee on Environment and Public Works
“Review of the President’s Climate Action Plan”

January 16, 2014

Good morning Chairman Boxer, Ranking Member Vitter, and Members of the Committee. I appreciate being invited here today to testify on this important topic.

Last year, the U.S. Government Accountability Office added climate change to its High Risk List, citing that it presents “a significant financial risk to the federal government.” According to the National Climatic Data Center, in 2012 weather and climate disaster events caused over $110 billion in damages, making it the second costliest year on record.

This Administration is committed to reducing the damage caused by climate change, and to preparing for its impacts, both in the long term as well as those we are already experiencing. In June 2013, the President reaffirmed this commitment with a Climate Action Plan that directs agencies to: cut carbon pollution; prepare for the impacts of climate change; and lead international efforts to address global climate change.

The U.S. General Services Administration (GSA) is one of the many Federal agencies doing its part to assist in this effort. As the landlord and caretaker of federal properties, GSA owns or leases 9,624 assets, which includes maintaining an inventory of more than 370 million rentable square feet of workspace, and preserving more than 481 historic properties. This large and diverse portfolio presents many opportunities for GSA to increase energy efficiency, reduce our contribution to climate change, save millions of dollars in energy costs and to plan and implement risk management.

As part of the President’s Climate Action Plan, GSA is improving the efficiency of our Federal buildings, identifying and preparing for climate risks, and working to ensure that we share lessons learned with our partner agencies.

Reducing Impact on Climate Change –

GSA reduces energy consumption across its portfolio through a variety of means. GSA leverages technology such as advanced metering, remote building analytics and smart building systems to uncover deeper energy savings opportunities. Advanced meters, which provide real time energy use information, have been installed in 450 buildings, representing 80% of GSA’s total electricity consumption metered. Continuous enhancements to the system, ongoing training of users, use of detailed historical data and expert modeling are all proven methods which are increasing energy efficiency at lesser cost.

GSA uses rapid building assessments to perform sophisticated energy audits that require no onsite work or new device installations. Such remote analytics have resulted in significant cost savings over traditional audits and have identified additional energy savings opportunities.

The President’s Climate Action Plan also highlights other important tools we can use to improve the efficiency of our buildings, including continued use of Energy Savings Performance Contracts (ESPCs). An ESPC engages the private sector in an agency’s efforts to achieve energy efficiency improvements. The private sector provides the upfront capital to make energy efficiency upgrades in a facility, and is paid by the Federal agency from the guaranteed energy savings under the contract. Once the contract ends, the agency continues to benefit from the reduced energy costs. In December 2011, the President challenged Federal agencies to enter into a combined $2 billion worth of ESPCs by December 31, 2013. GSA exceeded its own target of $175 million with $191 million in contracts awarded. These contracts, which range from 12 to 23 years in duration, are projected to reduce GSA’s annual energy consumption by 365 billion Btus, or about the amount of energy used in 3,380 single family homes per year, resulting in direct savings (lower utility payments) of $10.6 million per year.

The President’s Climate Action Plan sets new goals on the Federal use of Renewable Energy, increasing the current goal from 7.5 percent to 20 percent by 2020. In FY 2013, 46.1 percent of electricity procured or generated by GSA came from renewable sources (nearly 1,200 GWh). Over 24 GWh of this renewable electricity was generated at our own facilities. GSA expects to generate nearly 29 GWh per year once on-site renewable projects currently underway are fully operational. This amount of on-site renewable energy is enough to power nearly 2,600 homes.

Through the use of Green Button data, the President’s Climate Action Plan also highlights the importance of collecting data to promote better energy management. Green Button is an industry-led effort, in response to the Administration’s call-to-action, that looks to meet the challenge of providing electricity consumers with secure, easy to understand information on their energy usage. As directed in the December 2013 Presidential Memorandum on Federal Leadership in Energy Management, GSA will partner with the Department of Energy and Environmental Protection Agency to prepare and initiate a pilot Green Button initiative at Federal facilities. Following the pilot, DOE, in coordination with EPA, is required to issue guidance on use of the Green Button standard at Federal facilities. GSA will leverage the Green Button standard within its federal facilities to increase the ability to manage energy consumption, reduce greenhouse gas emissions, and meet sustainability goals.

Taken together, these efforts have led to a significant reduction in GSA’s energy use intensity and greenhouse gas emissions. In FY 2013, GSA achieved a cumulative reduction in energy usage per square foot of 24.8 percent,1 ahead of statutory targets. Since Fiscal Year 2011, these reductions have saved $192.7 million in avoided direct energy costs.2 Also, in FY 2013, GSA achieved an approximately 50 percent reduction in greenhouse gas emissions, exceeding our FY 2020 target.3 That is the equivalent of more than 60,000 homes powered for one year.

Preparing for the Impacts of Climate Change –

GSA is also preparing for the potential impacts of climate change as part of the President’s Climate Action Plan. While it is impossible to predict the precise occurrence and costs of each and every climate risk, it is imperative to develop a robust risk management approach.

One such area of focus has been preparing for future floods. GSA is actively coordinating with the U.S. Army Corps of Engineers (USACE), U.S. Global Change Research Program (USGCRP), Federal Emergency Management Agency (FEMA), National Oceanic and Atmospheric Administration (NOAA), and Federal Interagency Floodplain Management Task Force to incorporate the most recent and relevant flood-risk reduction strategies into GSA’s operations. We are in the process of updating GSA’s internal floodplain management guidance and are taking into consideration updated FEMA floodplain maps and additional guidance on using climate projections.

GSA is also working to boost the resilience of buildings and infrastructure. We are in the process of prioritizing our most mission critical and vulnerable facilities, looking into cost-effective climate-resilient investments, and investigating solutions that reduce both climate change risks and greenhouse gas emissions. A pilot project is currently in place to incorporate climate risk reduction factors into a new land port of entry facility. GSA will take lessons learned from this pilot and share with other agencies.

We believe these efforts will ensure GSA, and the Federal government broadly, is more prepared to address the long-term consequences of climate change.

Conclusion –

The President’s Climate Action Plan represents a commitment to reduce and respond to the impacts of climate change. As a major landholding agency of the Federal government, GSA plays an important role in mitigating and preparing for these adverse effects. Through improved energy efficiency and risk planning, we hope to continue to make progress on both of these critical efforts.

I am pleased to be here today, and I am happy to answer any questions you may have. Thank you.

Saturday, November 23, 2013

THUNDERSNOW: THE SOUND OF LAKE-EFFECT SNOW IN THE GREAT LAKES REGION

FROM:  NATIONAL SCIENCE FOUNDATION 
Scientists brave Old Man Winter to dig out secrets of lake-effect snows
'Tis the season...for snow.
Thundersnow.

Rare anywhere, thundersnow is sometimes heard during the lake-effect snowstorms of the Great Lakes. The interaction of clouds and ice pellets inside these storms generates a charge, with lightning and thunder the result.

How to catch thundersnow in action? This winter, stalwart veterans of tornadoes, hurricanes and other severe storms will be watching.

One is known as the Doppler-on-Wheels (DOW), a National Science Foundation (NSF) national facility used by NSF-supported and other researchers. Joining it is a University of Wyoming instrumented aircraft, the King Air, also an NSF-funded national facility.

In rain, sleet or snow, like the postman, they always deliver...storm data.

Using the DOW, the King Air and other equipment, scientists from across the country will converge on the shores of Lake Ontario from Dec. 5-21, 2013, and Jan. 4-29, 2014.

They will work to better understand the atmospheric conditions and mechanisms that lead to the deep snows that accumulate across the region each winter.

The project is called OWLeS (Ontario Winter Lake-effect Systems). OWLeS is funded by NSF and is a collaborative effort of nine universities.

Participating institutions are the University of Wyoming, University of Illinois, University of Utah, State University of New York (SUNY) Oswego, Hobart and William Smith Colleges, Millersville University, Penn State University, University of Alabama in Huntsville, SUNY Albany and the Center for Severe Weather Research (CSWR) in Boulder, Colo.

Although lake-effect snowstorms happen near all the Great Lakes, the New York area along Lake Ontario has some of the deepest snowfalls. Average annual snow reaches more than 100 inches. Nearby locations, such as the Tug Hill Plateau, may be blanketed with more than 250 inches each year.

But lake-effect snows aren't limited to the shores of Lake Ontario.

New York's Finger Lakes region also bears the brunt of lake-enhanced snowstorms. Complex interactions between the local environment and the far-reaching influence of Lake Ontario can significantly affect the location of lake-effect snowbands, says scientist Scott Steiger of SUNY Oswego.

"Even winter-hardened Great Lakes residents and infrastructure can be severely affected by heavy lake-effect snows," says Brad Smull, program director in NSF's Division of Atmospheric and Geospace Sciences, which funded the research.

"OWLeS' unique suite of modern mobile observing equipment and computer-based storm models will help us understand the processes that control the timing and location of these zones of heavy snow."

OWLeS scientists will use a network of specialized weather instrumentation--including three DOWs, the King Air, several weather balloon sounding systems, and a vertically-pointing radar wind profiler---to study the inner workings of lake-effect snowstorms.

The DOW and the King Air will intercept the lake-effect snowbands that cause the heavy snowfalls of the Lake Ontario region.

The King Air will fly over Lake Ontario, collecting data on snow and ice pellets, temperatures and other properties inside lake-effect snowbands.

The DOW looks more like the dish of a radio telescope than a sophisticated weather instrument. It's mounted on the back of a flat-bed truck. DOW-on-board, the truck becomes an odd configuration of generator, equipment and operator cabin.

Ungainly as it may appear, it's ideally suited to providing detailed information on the inner workings of snowstorms, says Josh Wurman, CSWR director.

The DOW uses Doppler radar to produce velocity data about objects--such as severe storms--at a distance.

"The King Air also carries Doppler radar that will transect the snowbands and a lidar that will show how the bands first form near the upwind side of the lake," says Bart Geerts of the University of Wyoming, co-lead scientist on the project with David Kristovich of the University of Illinois at Urbana-Champaign.

Lakes upwind of Lake Ontario can have a big influence on how heavily, and where, lake-effect snows fall.

"Air that has been moistened and mixed by moving over Lake Huron, Lake Michigan and even Lake Superior can play a major role in the large amount of snow that falls in the Lake Ontario snowbelt," says Kristovich.

Some of the questions scientists will investigate during OWLeS include:

What environmental factors have the greatest influence on the amount of snowfall and location of snowbands over and near Lake Ontario?

How do other Great Lakes affect the amount of snow that falls near Lake Ontario?

How does the interplay between winds and clouds produce long-lived snowbands far downstream of open water?

How does the local terrain influence the strength and longevity of these systems?

As snows begin to fall, the researchers will head out to collect data. The results will lead to increased predictability of, and preparedness for, Old Man Winter.

-NSF-

Thursday, November 21, 2013

MODIS IMAGE SHOWS LARGE ICEBERG SEPARATING FROM PINE ISLAND GLACIER IN ANTARCTICA

FROM:  NASA  
Pine Island Glacier 2013: Nov. 10

This MODIS image taken by NASA’s Aqua satellite on Nov. 10, 2013, shows an iceberg that was part of the Pine Island Glacier and is now separating from the Antarctica continent.  What appears to be a connection point on the top left portion of the iceberg is actually ice debris floating in the water.

The original rift that formed the iceberg was first observed in October 2011 but as the disconnection was not complete, the “birth” of the iceberg had not yet happened. It is believed the physical separation took place on or about July 10, 2013, however the iceberg persisted in the region, adjacent to the front of the glacier.
The iceberg is estimated to be 21 miles by 12 miles (35 km by 20 km) in size, roughly the size of Singapore. A team of scientists from Sheffield and Southampton universities will track it and try to predict its path using satellite data.  Image credit: NASA

Wednesday, November 20, 2013

TROPICAL CYCLONE 04B HEADS FOR SOUTHEASTERN INDIA

Right:  NASA's TRMM satellite saw broken bands of thunderstorms with moderate rainfall (yellow, orange) in the northern and eastern quadrants of Tropical Cyclone 04B on Nov. 19, 2013 in this image overlaid on ESA's METEO-7 Satellite.  Image Credit: NRL/NASA/ESA

FROM:  NASA 
Tropical Cyclone 04B Forms in Northern Indian Ocean
Cyclone 04B

NASA's TRMM satellite saw broken bands of thunderstorms with moderate rainfall (yellow, orange) in the northern and eastern quadrants of Tropical Cyclone 04B on Nov. 19, 2013 in this image overlaid on ESA's METEO-7 Satellite.
Image Credit: NRL/NASA/ESA.

The fourth tropical cyclone of the Northern Indian Ocean season formed and is headed for landfall in a couple of days in southeastern India. NASA's TRMM satellite saw broken bands of thunderstorms with moderate rainfall in the northern and eastern quadrants of Tropical Cyclone 04B on Nov. 19.

Tropical Cyclone 04B was located just 180 nautical miles south-southeast of Visakhapatnam, India near 15.0 north and 84.5 east at 1500 UTC/10 a.m. EST on Nov. 19. 04B had maximum sustained winds near 35 knots/40 mph/64 kph and is moving to the west at 8 knots/9.2 mph/14.8 kph.

Satellite imagery showed that the low-level center is organized and there is convection (building thunderstorms) flaring around the storm's center and there is broken bands of thunderstorms around the northern quadrant of the storm. TRMM satellite data showed rainfall rates were as high as 1.2 inches/30.4 mm per hour.
A microwave image from Nov. 19 at 1058 UTC/5:58 a.m. EST showed that the cyclone is well-defined and has curved bands of thunderstorms along the western quadrant.

The Joint Typhoon Warning Center or JTWC expects 04B to track slowly west slowly intensify before making landfall in India as a tropical storm. The JTWC expects landfall between Ongole south to Nellore, both cities in the southern India state of Andhra Pradesh late on Nov. 21.

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