PDF-INTERNATIONAL JOURNAL OF CLIMATOLOGY Int Climatol

COMRIE BRENT FRAKES and DAVID P BROWN Department of Geography En ironment Institute Pennsyl ania State Uni ersity Uni ersity Park PA USA Department of Geography and Regional De elopment Uni ersity of Arizona Tucson AZ USA Department of Geography So. J Climatol 2008 Published online in Wiley InterScience wwwintersciencewileycom DOI 101002joc1756 Consistency of modelled and observed temperature trends in the tropical troposphere B D Santer P W Thorne L Haimberger K E Taylor T 6 Africa Rainfall Climatology Version 2 Nicholas Novella 12 Wassila Thiaw NOAA NWS NCEP Climate Prediction Center Wyle Information Systems NOAA NWS NCEP Climate Prediction Center 1 INTRODUCTION In 1998 Data from two identical radiometers were analysed One instrument sampled the urbanised environment of Go 321teborg latitude 577057520N longitude 120057520E while the second one sampled a rural site Koster Island latitude 588357520N longitude 1100575 Researched by . Jesse Lundquist. Hourly temperature at SGF . November, 1911. Outline. Background. Gathering the data. Analyzing the data. Current results. Future work. From . Earthweek. : A Diary. of the Planet website. Sedimentary. Metamorphic. Rock. Very slowly weathered minerals. (e.g., quartz, muscovite). Slowly weathered minerals. (e.g., feldspars, biotite). Easily weathered minerals. (e.g., augite, hornblende, olivine). -5. -4. -3. -2. -1. 0. 1. 2. 0. 25. 50. 75. 100. 125. 150. 175. 200. 225. 250. Temperature Anomaly (. C. ). 160. 170. 180. 190. 200. Annual Solar Radiation (W. . m. -2. ). 0. 25. 50. 75. 100. 125. Anthony R. Lupo. 302 E ABNR Building. Department of Soil, Environmental, and Atmospheric Science . University of Missouri . Columbia, MO 65211. Phone: 573-884-1638 . Email: . LupoA@missouri.edu. Web.missouri.edu/~. What is the impact of ENSO Cycle?. Suzanne Fortin. Recent Annual Severe Weather Climatology. Distribution of of Severe Events During the Cold Season. Analysis of Severe Events and ENSO Cycle. Significance of ENSO Cycle to Severe Incidence. (q. over. ). Evapotranspiration (E). Precipitation (P). Groundwater. Soil. Bedrock. Outflow. (q. base. ). Topographic Divide. Inflow. (G. in. ). Figure 12.1. Ecological Climatology © 2008 G. Bonan. 200. Deningintegervalues,etc:-vali=3;vali=3:int-vals="abc";vals="abc":stringDeningfunctionvalues:-valinc=fn(x)=x+1;valinc=fn:int-int-inc(3);valit=4:int-valis_it_3=fn(x)=ifx=3then"yes"else"no";-is_it_3 *Correspondenceto:A.JohnArneld,DepartmentofGeography,TheOhioStateUniversity,154NorthOvalMall,Columbus,OH43210-1361,USA;e-mail:john.arneld@osu.edu2003RoyalMeteorologicalSociety A.J.ARNFIELDdrivenprog (Aug-Dec). . Monthly Forecast Verification. CRFS. December 8, 2015. Objectives. Analyze performance of ESP monthly volume forecasts. Baseflow. . period (August. -December. ). 1981-2010 ESP reforecasts; not official forecasts. Throughfall. Stemflow. Evaporation. Transpiration. Evaporation. Ocean . Lake. . Ground water. Overland. flow. Return. flow. Infiltration. Redistribution. Evaporation. Snow pack. Percolation. Capillary. trends. Anna A. . Shestakova. Obukhov. Institute of Atmospheric Physics, Moscow, Russia. Main goal:. Investigation of climatology of . extreme winds . in the Russian . Arctic. with special emphasis on .