PPT-On the estimation of land surface temperature from AMSR-E m

JeanLuc Moncet P Liang J Galantowicz G Uymin A Lipton C Prigent B Hornbuckle Atmospheric and Environmental Research Inc LERMA Iowa State University First version of global monthly. cisnagasakiuacjp Commission VIII8 KEY WORDS MODIS Land surface temperatureemissivity NDVINDWI ABSTRACT For the Land surface estimation from the satellite on the basis of the splitwindow method the land surface emissivity have to be the known value To Part I: Development w/o Earth rotation. A . sea-breeze. (or . onshore breeze. ) is a wind. . from the sea that develops over land. near coasts. . It is formed by increasing temperature differences between the land and water; . CloudSat. Matt . Lebsock. Chris . Kummerow. Motivation. Radiosonde. data [. Ohtake. , 1963. ]. Warm rain falls in all tropical ocean basins in all seasons more frequently than expected. Shipboard Weather Reports [. Neil Humpage, University of Leicester. The EO-Convoy Land study team. Introduction. ESA are undertaking three studies investigating possible . synergistic . satellite missions flying in formation with the operational . emissivities. with satellite-based estimates. C. Prigent and F. Aires (. Estellus. + . Observatoire. de Paris . ). P. Liang and J.-L. . Moncet. (AER). T. . Tian. (NASA). S. . Boukabara. (NOAA). Jean-Luc . Moncet. P. Liang, J. Galantowicz, G. Uymin, A. Lipton, C. Prigent*, B. Hornbuckle**. Atmospheric and Environmental Research, . Inc.. *LERMA. **Iowa State University. First version of global monthly. Dongdong. Wang, Tao He. Yi Zhang, Meredith Brown. Prof. Shunlin Liang. University of Maryland. May 21 2015. 1. Producing Incident Shortwave Radiation and . Photosynthetically. Active Radiation Products Over Land Surfaces . In the context of diagnosing the bias in the wintertime 2m air temperature and surface temperature over land in coupled RASM simulations, I have been looking more closely at whether the area that shows a temperature bias corresponds to any of the VIC soil or vegetation fields. There is definitely a well-defined area with enhanced downward . Latent and sensible heat. “Sweating”. Greenhouse Gases. Longwave. Radiation. Albedo. “Breathing”. “Reflectivity”. To better assess land-climate interactions in NH under future change scenarios, we are measuring greenhouse gas, energy, and radiation fluxes across 4 different land cover types that broadly represent the NH landscape: forest, field/pasture, corn/agriculture, residential/paved.  In the simplest terms, these fluxes can be thought of as breathing (respiring CO. local energy budgets . (mist, fog, dew, temperature inversions, land and sea breezes. ).. At the end of our third . lesson this week. I . will know . the three states in which moisture can be found in the atmosphere and understand the terms condensation, evaporation, . Distance from the equator. Ocean currents. Distance from the sea. Aspect. Orientation of mountain ranges. Altitude. Distance from the equator. TITLTED RAYS. VERTICAL RAYS. Atmosphere. diagonally rays. A process whereby liquid water is . converted to water vapour. and . removed from the vapour surface.. Evaporation consists of 2 components i.e. The energy component and the aerodynamic component. The energy component is responsible conversion of liquid water to water vapour. Embedded Flat Surfaces. From. . Scaled. . Orthographic. Image Data. Ricardo Ferreira. PhD. . Thesis. . Presentation. May 2010. Reconstruction of a . Sheet. of . Paper. From. Photos. Ricardo Ferreira. “Net rate of vapor transport to the atmosphere”. Reverse process of precipitation. Evaporation considered to be a problem for reservoirs storage on one hand may prove very valuable on the other hand .