2011
DOI: 10.5194/amt-4-1891-2011
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Retrieval of tropospheric water vapour by using spectra of a 22 GHz radiometer

Abstract: Abstract. In this paper, we present an approach to retrieve tropospheric water vapour profiles from pressure broadened emission spectra at 22 GHz, measured by a ground based microwave radiometer installed in the south of Bern at 905 m.Classical microwave instruments concentrating on the troposphere observe several channels in the center and the wings of the water vapour line (20-30 Ghz), whereas our retrieval approach uses spectra with a bandwidth of 1 GHz and a high resolution around the center of the 22 GHz … Show more

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Cited by 29 publications
(23 citation statements)
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References 33 publications
(29 reference statements)
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“…A tropospheric water vapour profile is also included in the forward model. The profile is obtained from the measured surface water vapour density at the ground (from a weather station), assuming a exponential decrease of the water vapour with altitude and a scale height of 2 km (Bleisch et al, 2011). Standard atmospheric profiles for summer and winter are considered for other species such as oxygen and nitrogen (Anderson et al, 1986); these profiles are incorporated into ARTS2.…”
Section: Methodsmentioning
confidence: 99%
“…A tropospheric water vapour profile is also included in the forward model. The profile is obtained from the measured surface water vapour density at the ground (from a weather station), assuming a exponential decrease of the water vapour with altitude and a scale height of 2 km (Bleisch et al, 2011). Standard atmospheric profiles for summer and winter are considered for other species such as oxygen and nitrogen (Anderson et al, 1986); these profiles are incorporated into ARTS2.…”
Section: Methodsmentioning
confidence: 99%
“…In the forward model a water-vapor profile with an exponential decrease is included. This profile is calculated with the measured surface water vapor density from the ExWiWeather station (placed next to TEMPERA) and assuming a scale height of 2000 m. Further descriptions can be found in Bleisch et al (2011). For other species like oxygen (O 2 ) and nitrogen (N 2 ) we used standard atmospheric profiles for summer and winter, which are incorporated into ARTS2 (middle latitude FASCODE (Fast Atmospheric Signature CODE) (Anderson et al, 1986)).…”
Section: Forward Model Parametersmentioning
confidence: 99%
“…A tropospheric water vapour profile with an exponential decrease is included. This profile is calculated with the measured surface water vapour density from the ExWi weather station (placed next to TEMPERA) and assuming a scale height of 2000 m (Bleisch et al, 2011). For other species like oxygen (O 2 ) and nitrogen (N 2 ) we used standard atmospheric profiles for summer and winter (Anderson et al, 1986), which are incorporated into ARTS2.…”
Section: Retrievalmentioning
confidence: 99%