Speaker
Dr
Georg Heygster
(University of Bremen, Germany)
Description
Atmospheric water vapor is an important constituent of the global hydrological cycle; it transports humidity and heat and it is the most important greenhouse gas. While over open ocean total precipitable water vapor (PW) is routinely surveyed with satellite microwave imagers like SSMI(S) and AMSR-E/2, large-scale observations in polar regions with low water vapor burden are much more difficult because of the low water vapor signal and, over sea ice and land ice, the high and highly varying surface emissivity. However, a procedure has been suggested exploiting the data of the satellite humidity sounders SSM/T2, AMSU-B and MHS aboard the DMSP, Aqua and Metop satellites or satellite series, respectively.
The basic idea is to use three channels of neighbouring frequencies. The surface contribution in the observed brightness temperatures is excluded by considering the ratio of brightness temperature differences. The resulting quotient is closely related to the atmospheric opacity from which in turn the PW can be inferred. The original version [1] used the three dual-band channels centred around the water vapor absorption line near 183 GHz (183 ± 3, ± 5, and ± 7 GHz) plus the 150 GHz channels in two different 3-channel combinations for the ranges 0 to 1.5 kg/m2 and 1 to 7 kg/m2, resp.. Later, the procedure has been adapted to the microwave humidity sounders AMSU-B and MHS with channels at 183 ± 1, ± 3, and ± 7 GHz [2]. Moreover, the method has been extended to also use the 89 GHz channel by introducing knowledge about the emissivity of Arctic sea ice. This allows for a retrieval up to 14 kg/m2. Results for Antarctica based on the original algorithm will be presented, including two years (2006-2007) of new data. In coastal Antarctic areas, Global Positioning System (GPS) and radiosounding (RS) stations are available and their long time series of observations can be used to retrieve PW. To ensure the utmost accuracy of the results homogeneous, consistent and up-to-date processing strategies for these data-sets were adopted and the content and variations of the PW were obtained at five Antarctic sites (Negusini et al 2016). The resulting time series will be compared to satellite based retrievals at the places of the stations. After correcting the satellite based retrievals based on the comparisons with the GPS and radiosonde based PW observations at the places of the stations, the satellite data will be used to extend the PW retrieval over whole Antarctica.
References
1. Miao, J., K. Kunzi, G. Heygster, T. A. Lachlan-Cope, J. Turner, 2001: Atmospheric water vapor over Antarctica derived from SSM/T2 data. J. Geophys. Res., 106, D10 (May 27), 10187--10203.
2. C. Melsheimer, G. Heygster 2008: Improved retrieval of total water vapor over polar regions from AMSU-B microwave radiometer data. IEEE Trans. Geosci. Remote Sens. 46(8), p.2307-2322, doi:10.1109/TGRS.2008.918013.
3. Negusini M, Petkov BH, Sarti P, and Tomasi C. 2016. Ground based water vapor retrieval in Antarctica: an assessment. IEEE Trans. Geosci. Remote Sens. (TGRS) 54 (5), p. 2935-2948, doi:10.1109/TGRS.2015.2509059.
Primary author
Dr
Georg Heygster
(University of Bremen, Germany)
Co-authors
Dr
Arantxa Triana Gómez
(University of Bremen)
Dr
Christian Melsheimer
(University of Bremen)
Dr
Gunnar Spreen
(University of Bremen)
Dr
Monia Negusini
(Institute of Radio Astronomy – INAF)
