Office of Biological and Environmental Research Weekly Report

March 16, 2009

 

Remote Detection of Drizzle from Low Altitude Clouds.  DOE scientists developed a novel remote sensing method to detect drizzle from low-altitude water clouds using the Atmospheric Radiation Measurement (ARM) program millimeter wave cloud radar (MMCR).  Low-altitude water clouds have a significant influence on earth’s climate through their interaction with radiation to and away from the earth.  It has been a major technical challenge to remotely determine if low-altitude clouds do or do not rain because of the low thermal contrast between these clouds and earth’s surface.  ARM investigators found that cloud drizzle is dictated by the vertical variation of rain drop size and total cloud water.  Drizzling clouds usually exhibit a decreasing trend of rain droplet size with altitude, while non-drizzling clouds have an opposite trend.  Both theoretical analyses and observations suggest that drizzle drops can significantly increase in size near the bottom of a cloud layer. These findings help improve remote sensing of precipitation amounts and understanding of aerosol effects on clouds, associated rain, and climate.

 

Reference:

Chen, R, R Wood, Z Li, R Ferraro, and F Chang, 2008: "Studying the vertical variation of cloud droplet effective radius using ship and space-borne remote sensing data." Journal of Geophysical Research 113, doi:10.1029/2007JD009596.

Media Interest: No

Contact: Kiran Alapaty, SC-23.1, (301) 903-3175

 

Estimating Fossil Energy-based CO2 Emissions from US Croplands:  DOE supports research to understand mechanisms of carbon sequestration in managed ecosystems.  An important part of that research is knowing the sources of carbon emissions.  Scientists from Oak Ridge National Laboratory report a method to estimate both on- and off-site fossil energy-based CO2 emissions (FCE) associated with crop production.  FCE was found to differ by crop and region because of changes in energy requirements for crop production driven by environmental differences, e.g., soil texture, soil chemistry, and climate.  Changes in policies (e.g., Farm Bills) and abrupt changes in annual weather patterns (e.g., droughts and wet years) have also resulted in annual shifts in FCE.  This new method is important because estimates of fossil-fuel consumption for cropping practices and the associated CO2 emissions enable (i) monitoring of energy and emissions with changes in land management and (ii) calculation and balancing of regional and national carbon budgets.

 

Reference:  Nelson, R.G., C.M. Hellwinckel, C.C. Brandt, T.O. West, D.G. De La Torre Ugarte, G. Marland. 2009. Energy Use and Carbon Dioxide Emissions from Cropland Production in the United States, 1990-2004. Journal of Environmental Quality 38: 418-425.

 

Media interest:  No

Contact:  Mike Kuperberg, SC-23.1, (301) 903-3511; Roger Dahlman, SC-23.1, (301) 903-4951