PPT-Assessing the impact of representing snow-albedo feedback on the response of hydrology

Downscaling methods LOCA Pierce et al 2014 Retains GCMprojected precipitation changes as a ratio Preserves observed number of dry days in historical period Preserves mean changes Bias corrects for lowfrequency variability. James . Lazarcik. . 1, 2. , Jacqueline . Amante. . 1, 2. , . Alden Adolph. 3. ,. . Mary Albert. 3. , Jack . Dibb. . 1, 2. , Cameron Wake. . 1, 2. 1 . Department of Earth Science , University of New Hampshire, Durham, NH, USA. Ned Bair . US Army Corps of Engineers Cold Regions Research and Engineering Laboratory. Earth Research Institute, UC - Santa Barbara. 1. Heat transfer. Radiation. Energy transfer via photons. Sensible. at UNR. 29 July 2013. By Pat Arnott. Computer to read spectrometer data.. Spectrometers are at . Dambar’s. left hand.. Irradiance sensor. (looks up). Radiance sensor. (looks down). Bryan steadies the albedo measuring device. 2. Aaron Donohoe, University of Washington. CLIVAR CONCEPT HEAT Meeting. Exeter, September 30, 2015 . Energy imbalance and temperature change. ASR . =. . OLR. Unperturbed. Atmospheric Emission Level. Module 13 -14. pg. 175 - 185 . Shelita McCadney. Teacher Quality Team. 601.863.6399. Research says…. Setting Objectives and Providing Feedback. *Yields a 23 percentile gain. iBelieve, iPractice. 3. Ned Bair . US Army Corps of Engineers Cold Regions Research and Engineering Laboratory. Earth Research Institute, UC - Santa Barbara. 1. Heat transfer. Radiation. Energy transfer via photons. Sensible. BROMLEY NORTH STATION – . Planning Policy REVIEW. Presentation BRRA . – . 26. th. July 2016. The Site . A complex but underutilised site – multiple stakeholders – NR/Tfl/LBB/SE Trains/NHS. Near nadir imagers do not provide the multi-angle observations necessary to capture the multi-angle reflective character described by the surface BRDF. Therefore, the Landsat albedo algorithm couples atmospherically corrected 30m Landsat . Marschke. , Southwest Early College. Different Forms of Elements. Elements are always pure, but do not always look the same. Example: carbon. graphite. diamond. Forms of carbon, cont.. BLACK CARBON. Sounder Radiances . using . Forecast . Sensitivity to . Observation Impact . (FSOI) Metrics. Will McCarty. 1. , Dan Holdaway. 2. , and Ron Gelaro. 1. Global Modeling and Assimilation Office. 1. NASA Goddard Space Flight Center. AERosol. AND CLOUD . RETRIEVALS OVER SNOW. Kokhanovsky. VITROCISET Belgium SPRL, . Bratustrasse. 7, 64289 Darmstadt, Germany. a.kokhanovsky@vitrocisetbelgium.com. . CLOUD. AEROSOL. CONCLUSIONS. CLOUDS. MEASURING IMPACT EX-POST The Checklist describes what needs to be assessed ex ante and measured ex post to assess impact in 7 key areas using the Global Impact Investing Network146s GIIN IRIS framewor . Albedo increases due to more ice coverage to something like about 0.35 which is then equivalent to a 6% change (3 % change in mean geometric distance from the Sun). Qualitative Albedo Feedback loop:. Lecture 3 – . Forcings. and Feedback. Outline of course. Do we understand the science behind climate change?. Historical climate. Basics of climate science. Modeling the climate. Understanding the .