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Subsidence of high atmospheric air above the Arctic derived from CO time series measured by ground-based microwave radiometers.

Applicant Dr. Mathias Palm
Subject Area Atmospheric Science
Term from 2008 to 2013
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 65226577
 
Final Report Year 2013

Final Report Abstract

In the project a data analysis chain for millimeterwave spectra measured using the KIMRA instrument in Kiruna (68 degrees North) was successfully set up. They found, that the results obtained from the measurements of the KIMRA instrument are in good agreement to existing satellite measurements, namely from the MLS instrument on the AURA satellite and the MIPAS instrument on Envisat. The results were used to validate the newly developed SD-WACCM model. The major findings were that the SD-WACCM model were able to model the CO content of the mesosphere to surprisingly good degree. Surprisingly good, because 1) the model is a global circulation model nudged to a meteorological analysis up to 50 km, 2) the comparison took place at a particular place on earth and 3) the comparison took place at 60 to 70 km, well above the altitude where the nudging has a direct effect. One of the conclusion is accordingly, that dynamics of the mesosphere are determined mainly from below. Inconsistencies in the dynamics could be explained by the fact, that the wave propagation, which provides the link between the stratosphere and the parts of the atmosphere above the stratosphere is only modeled in a statistical sense. The results and experience of Dr. Hoffmann could be used to devise a new instrument to measure the CO content of the mesosphere and to continue this research.

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