PPT-Precipitation
Author : briana-ranney | Published Date : 2016-03-03
Interception Throughfall Stemflow Evaporation Transpiration Evaporation Ocean Lake Ground water Overland flow Return flow Infiltration Redistribution Evaporation
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Precipitation: Transcript
Interception Throughfall Stemflow Evaporation Transpiration Evaporation Ocean Lake Ground water Overland flow Return flow Infiltration Redistribution Evaporation Snow pack Percolation. Isaac Morgan, Elizabeth Tanner, Jeff Monroe, Jason . Behrends. University of Wisconsin- Platteville Biology Department. Introduction. Methods. Results. Conclusions. References . Used . Riveredge. CBC data from 1977 to 2011 on European Starling, American Robin, American Crow, Horned Lark, Great Horned Owl and Black-Capped Chickadee and . Cloud Naming. Prefix indicates height. Cirro. . high, 5-13 km. Alto middle, 2-5 km. (none) low, 0-2 km. Name for appearance. Cirrus . wispy strands. Stratus layered, uniform. Cumulus puffy with vertical structure. Precipitation Processing System (PPS. ). GPM Mission Gridded Text Products . Provide Surface Precipitation Retrievals. Erich Franz . Stocker. , O. Kelley, C. . Kummerow. , G. . . Huffman. , . W. Olson, J. Kwiatkowski . What is precipitation?. Water that falls from the sky, it can be in different forms.. Hail, sleet, snow, rain.. Rain. As warm air rises into the atmosphere it cools. The air creates water vapor which condenses and forms into clouds. Once the clouds are big enough and are holding enough water it begins to rain.. . Photograph: Tony Clarke, VOCALS . REx. flight RF07. Robert Wood. University of Washington. Dave Leon and Jeff Snider, University of Wyoming. Radiative. impact of cloud droplet concentration variations. Learning objectives. Be able to estimate area average precipitation from point measurements using a variety of methods. Estimate design rainfall amounts and intensities. Develop ArcGIS skills for analysis . Caitlin Gorden, Jamie Jefferson, James Nooyen Jr.. University of Wisconsin-Platteville. The Christmas Bird Count started on Christmas day in 1900 to prevent widespread shooting of . birds, and promote . Water vapor, droplets of water suspended in the air, builds up in the Earth's atmosphere. . Water vapor in the atmosphere is visible as clouds and fog. . Water vapor collects with other materials, such as dust, in clouds. Precipitation condenses, or forms, around these tiny pieces of material, called cloud condensation nuclei (CCN).. Crown King. May Average: 0.30”. June Average: 0.26”. July Average: 3.44”. August. . Average: . 3.34”. Crown King 2016 . (. 86. % . of . average. ). May: 1.20”. June: 0.36”. July: 1.60”. Idar Barstad. Idar.Barstad. @uni.no. Uni Research – (. UniComputing / Bjerknes Centre for Climate Research). Motivation: . Orographic precipitation and climate change. Results from a small-scaled field campaign. Artificial rain making.. Process of Precipitation:. Precipitation is caused by condensation of water . vapours. of the air mass. . The ascending air mass with sufficient amount of water . vapours. becomes saturated due to adiabatic cooling. Condensation of water . Precipitation can be divided into three categories. . based on whether it falls as liquid water, liquid water that freezes on contact with the surface, or . ice. Mixtures of different types of precipitation, including types in different categories, can fall simultaneously. . Mountains Experiment (OLYMPEX). Lynn McMurdie . University of Washington. (co-authors: Angela Rowe, Joe . Zagrodnik. ,. Stacy . Brodzik. , . Thomas . Schuldt. , Robert . Houze. . and. , . Jamin. . Kengo. . Matsubayashi. Japan Meteorological Agency. The Met Office. Outline. Motivation. Observation and evaluation method. Evaluation result. Summary. In many convection schemes, water substances are empirically modelled..
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