PDF-NOHRSC OPERATIONS AND THE SIMULATION OF SNOW COVER PROPERTIES FOR THE COTERMINOUS US

The National Weather Service NWS provides timely and accurate hydrologic warnings forecasts andplanning information to ensure the safety of the population mitigate property losses and improve th. Lessons Learned. HPC Surface Analysis, Monday 12Z. Forecast Concern- Precip Type. 850 mb Analysis, Monday 12z. Forecast Concern- Precip Type. 850 mb Analysis, Tuesday 00z. National Radar 11:30Z. National Radar 18:30Z. CMP: 2 or 4 cores, 3.2GHz ROB size: 128 Fetch/Exec/Retire/Commit width: 4 / 7 / 5 / 3 Branch predictor: G-share, 64KB, 4K BTB Branch misprediction penalty: 10 cycles Processor side prefetcher: Stride Jiang . Zhu. 1. . and Chuck . Lindsay. 2. 1. Geographic Information Network of Alaska, University of Alaska Fairbanks . -. jiang@gina.alaska.edu | . 2. Inventory and Monitoring Program, National Park Service - chuck_lindsay@nps.gov. Snowfall, Snow melt and Thermal Belts. Gina Loss – Service Hydrologist. Dave Bernhardt – Science & Operations Officer. Great Falls, Montana. Why MODIS to monitor snow and river ice?. Montana is rural with a low population density. 01-02-2012. Uintah Basin Applied Tech College Vernal Utah 1 January 2013 ~11:30 am. Topics. Snow cover analysis. Weather analysis of last few days . Weather forecasts for next week. MODIS Visible Imagery Last 3 Years. Improving Driver Ability to Avoid Collisions When Following a Snowplow. Michele Olsen, . Siddharth. . Deokar. , . and Peter . Willemsen. Department of Computer Science. University of Minnesota Duluth. CPA-A produces more accurate chlorophyll in both nearshore and offshore. Operational Algorithms for the Retrieval of Water . Quality Parameters in the Great Lakes from Satellite Data. . Robert Shuchman. Eduard Fast. Content. Motivation. Why EM simulation. Basics. Signal Integrity. S-Parameters. Advanced Design Systems (ADS). Why ADS?. General Simulation process. Three key EM simulation technologies. Cryosphere Products Validation Team. Jeff Key, NOAA/NESDIS/STAR, Team Lead. Paul Meade, Cryosphere Products JAM. DR # 7132. CCR # 474-CCR-13-0945. DRAT discussion: April 19, 2013. AERB presentation: April 24, 2013. and subtract Examples if 8 3 11 is known then 3 8 11 is also known Commutative property of additionTo add 2 6 4 the second two numbers can be added to make a ten so 2 6 4 2 10 12 Associativ C. CHABAL, V. PERROT. CEA. Caroline.chabal@cea.fr. For . the past 10 years, the CEA has been developing iDROP, a VR based software, which offers a support to prepare scenarios, optimize studies, and train future workers. . . Kat J. Bormann, Jet Propulsion Laboratory, Caltech . Data & Results: . There is extensive surface and satellite-based evidence of significant declines in Northern Hemisphere spring snow cover starting in the mid 1980’s in response to recent warming. However, our ability to monitor snow cover and trends in mountain regions is severely hampered by limitations in current satellite systems. Consequently the trends in the mountains are much less clear.. What have we learned from observations and CMIP5 simulations?. Chris . Derksen. and Ross Brown. Climate Research Division. Environment . Canada. Thanks to our data providers. :. Rutgers Global Snow Lab . EURO-CORDEX regional climate models with . MODIS remote sensing observations . for the European Alps. M. Matiu, M. Petitta, C. Notarnicola, M. Zebisch. Eurac Research, Bolzano, Italy. Motivation. Traditional .