Radon Measurements of Atmospheric Mixing (RAMIX) 2006–2014 Final Campaign Summary
Uncertainty in vertical mixing between the surface layer, boundary layer, and free troposphere leads to large uncertainty in “top-down” estimates of regional land-atmosphere carbon exchange (i.e., estimates based on measurements of atmospheric CO2 mixing ratios). The radioisotope radon-222 (222Rn) is a valuable tracer for measuring atmospheric mixing because it is emitted from the land surface and has a short enough half-life (3.8 days) to allow characterization of mixing processes based on vertical profile measurements.
- Lawrence Berkeley National Laboratory
- National Oceanic and Atmospheric Administration
- Publication Date:
- OSTI Identifier:
- Report Number(s):
- DOE Contract Number:
- Resource Type:
- Program Document
- DOE ARM Climate Research Facility, Pacific Northwest National Laboratory; Richland, Washington.
- Research Org:
- DOE Office of Science Atmospheric Radiation Measurement (ARM) Program (United States); Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
- Sponsoring Org:
- USDOE Office of Science (SC), Biological and Environmental Research (BER) (SC-23)
- Country of Publication:
- United States
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