Middle Atmospheric Water Vapour Radiometer (MIAWARA):: Validation and first results of the LAPBIAT Upper Tropospheric Lower Stratospheric Water Vapour Validation Project (LAUTLOS- WAVVAP) campaign -: art. no. D13306

被引:26
作者
Deuber, B
Ilaefele, A
Feist, DG
Martin, L
Kämpfer, N
Nedoluha, GE
Yushkov, V
Khaykin, S
Kivi, R
Vömel, H
机构
[1] Univ Bern, Inst Appl Phys, CH-3012 Bern, Switzerland
[2] USN, Res Lab, Washington, DC 20375 USA
[3] Russian Fed Serv Hydrometeorol & Environm Monitor, Cent Aerol Observ, Moscow 141700, Russia
[4] Finnish Meteorol Inst, Arctic Res Ctr, FI-99600 Sodankyla, Finland
[5] Univ Colorado, Cooperat Inst Environm Sci, Boulder, CO 80309 USA
关键词
D O I
10.1029/2004JD005543
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
We present a validation study for the ground-based Middle Atmospheric Water Vapour Radiometer (MIAWARA) operating at 22 GHz. MIAWARA measures the water vapor profile in the range of 20-80 km. The validation was conducted in two phases at different geographical locations. During the first operational period the radiometer was operated at middle latitudes in Bern, Switzerland, and the measured water vapor profiles were compared with the HALOE satellite instrument. The agreement between HALOE and MIAWARA was for most altitudes better than 10%. In the second comparison phase, MIAWARA took part in the Lapland Atmosphere-Biosphere Facility (LAPBIAT) Upper Tropospheric Lower Stratospheric Water Vapour Validation Project (LAUTLOS-WAVVAP) campaign in early 2004 in the subarctic region of northern Finland. During this campaign, different balloon sondes probed the water vapor content in the upper troposphere and lower stratosphere. The stratospheric water vapor profiles of the fluorescent hygrometer FLASH-B and the NOAA frost point hygrometer mirror in the range of 20-26 km were compared with the lowermost retrieval points of MIAWARA. The agreement between the balloon instruments and MIAWARA was better than 2% for a total number of 10 comparable flights. This showed the potential of MIAWARA in water vapor retrieval down to 20 km. In addition, the northern Finland MIAWARA profiles were compared with POAM III water vapor profiles. This comparison confirmed the good agreement with the other instruments, and the difference between MIAWARA and POAM was generally less than 8%. Finally, the tipping curve calibration was validated with tipping curve measurements of the All-Sky Multi Wavelength Radiometer (ASMUWARA) which was operated 10 months side by side with MIAWARA. The agreement of the tropospheric opacity derived from these tipping curves agree within 1%.
引用
收藏
页数:10
相关论文
共 43 条
[1]   ARTS, the atmospheric radiative transfer simulator [J].
Buehler, SA ;
Eriksson, P ;
Kuhn, T ;
von Engeln, A ;
Verdesa, C .
JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER, 2005, 91 (01) :65-93
[2]  
BUTCHART N, 1986, J ATMOS SCI, V43, P1319, DOI 10.1175/1520-0469(1986)043<1319:TAOTSP>2.0.CO
[3]  
2
[4]  
Calisesi Y, 2003, J ATMOS OCEAN TECH, V20, P1543, DOI 10.1175/1520-0426(2003)020<1543:IOSUIB>2.0.CO
[5]  
2
[6]   A new 22-GHz radiometer for middle atmospheric water vapor profile measurements [J].
Deuber, B ;
Kämpfer, N ;
Feist, DG .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2004, 42 (05) :974-984
[7]   Minimized standing waves in microwave radiometer balancing calibration -: art. no. RS1009 [J].
Deuber, B ;
Kämpfer, N .
RADIO SCIENCE, 2004, 39 (01)
[8]   Qpack, a general tool for instrument simulation and retrieval work [J].
Eriksson, P ;
Jiménez, C ;
Buehler, SA .
JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER, 2005, 91 (01) :47-64
[9]   The 22 GHz radio-aeronomy receiver at onsala space observatory [J].
Forkman, P ;
Eriksson, P ;
Winnberg, A .
JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER, 2003, 77 (01) :23-42
[10]  
GODSON WL, 1962, J R METEOROL SOC, V88, P229