PDF-California is suffering from a third year of drought with nearrecordlow reservoirs mountain

As a direct result far less water than usual is available for cities farms and natural ecosystems There are farreaching effects that will intensify if dry conditions persist Several response strategies are available that will provide both nearterm r. Kevin E Trenberth. NCAR. Warmer air holds more moisture. 4% per °F. Global warming=. More heat .  . More drying. . More . evaporation. . More moisture. More rain. More drought. Drought. Sam Sartwell, . Winter Ecology, EBIO 4100, Spring 2014, CU Mountain Research Station, CU Boulder. Putting this question in a winter ecological perspective. The purpose of the study is to understand the differences in the snowpack between these two areas. . RADIOMETRY. A. W. (Tony) . England, Hamid . Nejati. , and Amanda Mims. University of Michigan, Ann Arbor, Michigan, U.S.. A. IGARSS 2011. . Outline. Intro to global snowpack sensing. Limitations of current snowpack sensing technologies. Reading: Applied Hydrology Sections 5.6 to 5.8 and Chapter 6 for Tuesday of next week. Runoff. Streamflow. Generation. Excess Rainfall and Direct Runoff. SCS Method for runoff amount. Examples from Brushy Creek. NCEP. North . American Land Data Assimilation (NLDAS. ):. Implications and Challenges . of. Extending . the Length of the . Climatology. by. Youlong Xia. 1. and Bala Narapusetty. 2. . Learning objective. Be able to calculate infiltration, infiltration capacity and runoff rates using the methods described in the Rainfall Runoff workbook chapter 5 and . Dingman. . chapter 6.. Problem 1 as an example. Baseflow. Separation. Phi-Index. Determining the .  index and Excess Rainfall Hyetograph. Direct Runoff from . the SCS Curve Number Equation. Midterm Format. Open Book. . Answer all questions. Please answer on separate sheets of paper. You may refer to the textbook, notes, solutions to . Authors: Anne F. Van Loon et al (Nature, Feb 2016). Kimberly Duong. March 1, . 2016. Background. This paper describes:. human influences on drought. potential feedbacks between drought and society. Land use changes by humans alter hydrologic processes (evapotranspiration, infiltration, surface runoff, . Where Germs Live. Session 1. Agenda. Welcome. Welcome and Introductions. Four Body Reservoirs. Word Clouds and Discussion. Bringing It Together. Conclusion. Four Body Reservoirs. What Do You Think?. The Body Reservoirs. Runoff may be defined as that part of precipitation as well as any other flow contributions which appear in surface streams of either perennial or seasonal nature.. It is the flow collected from a drainage basin appearing at the outlet of the basin or catchment. Rolf Reichle. 1. , Gabrielle DeLannoy. 1,2. , and . Wade Crow. 3. 1. NASA Goddard Space Flight Center Global Model and Assimilation Office. 2 . University of Louvain, Louvain, Belgium. 3. USDA ARS Hydrology and Remote Sensing Lab. Learning objectives. Be able to define and compute the topographic wetness index and describe its role and use in TOPMODEL runoff calculations. Be able to use TOPMODEL principles to calculate the spatial distribution of soil moisture deficit and use this information in the calculation of runoff using appropriate GIS tools. Tagele. . Mossie. Aschale. 1. ,. . David J. Peres. 1 . , . Nunziarita. Palazzolo. 1. , Guido Scuito. 2. , Antonino Cancelliere. 1. University of Catania, Department of Civil Engineering and Architecture, Catania, Italy (tagele.aschale@phd.unict.it) . Wolfgang Wagner. Department of Geodesy and . Geoinformation. (GEO). Vienna University of Technology (TU Wien). http://www.geo.tuwien.ac.at/. Active and Passive . Microwave . Remote Sensing. Passive microwave sensors record .