PPT-Estimating snow-cover trends from space

Kat J Bormann Jet Propulsion Laboratory Caltech Data amp Results There is extensive surface and satellitebased evidence of significant declines in Northern Hemisphere spring snow cover starting in the mid 1980s 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. Snow Cover . Runoff Modeling. By Almoutaz Abdalla. Snow Cover, SWE and Runoff Modeling. Introduction. Snow Water Equivalent (SWE). Remote Sensing in Hydrological modeling (snow dominated). Components of Snowmelt modeling. Evan Esfahani. Winter Ecology 2014 Mountain Research Station. Introduction. The relationship between vegetation density and canopy cover influences snowpack and how it accumulates/depreciates.. Accumulation of snow under forest canopies will decline with increased canopy cover because of sublimation and interception in canopy (Pomeroy, 2002). . 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. 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. Functions – graphing/tables. MATHO . QUESTION 1. Make a function table.. Input. y = 3x + 2. Output. 0. 1. 2. 3. cover space c. . Input. y = 3x + 2. Output. 0. 3. . • 0 + 2. Evan Esfahani. Winter Ecology 2014 Mountain Research Station. Introduction. The relationship between vegetation density and canopy cover influences snowpack and how it accumulates/depreciates.. Accumulation of snow under forest canopies will decline with increased canopy cover because of sublimation and interception in canopy (Pomeroy, 2002). . 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. NOAA AMSR2 SNOW AND ICE PRODUCTS Jeff Key NOAA/NESDIS Madison, Wisconsin USA AMSR-2 Snow and Ice Products Snow Cover (SC) – Presence/absence of snow Snow Depth (SD) – The depth of snow on land Session 4 Estimating Nitrogen Credits Outline Factors effecting nitrogen content of cover crop Factors effecting cover crop nitrogen availability to cash crop Major steps to estimating nitrogen credits 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. Tropical . Cryosphere. Workshop. Morocco. . s. pecific. . presentation. Meriem ALAOURI . CNC/DMN. Arusha, 4 July 2017. Geographical. . context. Mountains cover more than two thirds of the Moroccan territory and reach significant heights. . into . NCEP . Operational CFS/GFS System. Michael B. . Ek. and . Jiarui. Dong. NOAA/NCEP/EMC, College Park, Maryland, USA. STAR JPSS Science Team Meeting. August . 17, . 2017, NCWCP, College Park MD. 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 .