Global Fire Emissions and Fire Effects on Biophysical Properties and the Associated Radiative Forcing Yufang Jin 1, James Randerson 1, G. R. van der Werf.
Aerosol Black Carbon Transport to Antarctica Image background: London at Night BLACK CARBON Signal of global pollution and its impact on ice masses Jefferson.
NATIONAL INSTITUTE OF METEOROLOGY AND HYDROLOGY – BULGARIAN ACADEMY OF SCIENCES 15 th EMS Annual Meeting & 12 th European Conference on Applications of.
1.Solar-Terrestrial Influences Laboratory, BAS, Department Stara Zagora, Stara Zagora, Bulgaria 2. Solar-Terrestrial Influences Laboratory, BAS, Sofia,
Advanced SynopticM. D. Eastin Midlatitude Cyclogenesis.
1 Application of Satellite Land Measurements in Improving NCEP Numerical Weather Prediction Weizhong Zheng, Michael Ek, Helin Wei, Jesse Meng, Jiarui Dong.
MET 112 Global Climate Change – Lecture 11 Observations of Recent Climate Change Dr. Craig Clements San Jose State University Outline How do we observe?
1 Radiative Effect of Clouds on Tropospheric Chemistry in a Global 3-D Chemical Transport Model Hongyu Liu (hyl) National Institute.
Land-surface-BL-cloud coupling Alan K. Betts Atmospheric Research, Pittsford, VT [email protected] Co-investigators BERMS Data: Alan Barr, Andy Black, Harry.
Basic definitions: Evapotranspiration: all processes by which water in liquid phase at or near the earth’s surface becomes atmospheric water vapor “Evaporation”
Soil Carbon in Global Perspective Two main anthropogenic C inputs are form fossil fuel and soil/plants Main C sinks are atmosphere, oceans and (???) ecosystems.
Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more radiation reflected by the surface Albedo, together.