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61.
Global monitoring of tropospheric water vapor with GPS radio occultation aboard CHAMP 总被引:1,自引:0,他引:1
S. Heise J. Wickert G. Beyerle T. Schmidt Ch. Reigber 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2006,37(12):2222-II
The global positioning system radio occultation (GPS RO) technique provides a powerful tool for atmospheric sounding which requires no calibration, is not affected by clouds, aerosols or precipitation, and provides an almost uniform global coverage. The paper deals with application of GPS RO measurements from CHAllenging Minisatellite Payload (CHAMP) for the retrieval of tropospheric water vapor profiles. CHAMP RO data are available since 2001 with up to 200 high resolution atmospheric profiles per day. We introduce a new direct method for water vapor retrieval from GPS RO data. Additionally, a 1Dvar algorithm is used for this purpose. The so derived CHAMP water vapor profiles are validated with radiosonde data on a global scale. Here, both methods come to statistically comparable results revealing a negative bias of less than 0.1 g/kg and a standard deviation of less than 1 g/kg specific humidity in the mid troposphere. Potentials of CHAMP RO retrievals for monitoring the mean tropospheric water vapor distribution on a global scale are presented. 相似文献
62.
M. Schmidt D. Bilitza C.K. Shum C. Zeilhofer 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2008
The knowledge of the electron density is the key point in correcting ionospheric delays of electromagnetic measurements and in studying the ionosphere. During the last decade GNSS, in particular GPS, has become a promising tool for monitoring the total electron content (TEC), i.e., the integral of the electron density along the ray-path between the transmitting satellite and the receiver. Hence, geometry-free GNSS measurements provide informations on the electron density, which is basically a four-dimensional function depending on spatial position and time. In addition, these GNSS measurements can be combined with other available data including nadir, over-ocean TEC observations from dual-frequency radar altimetry (T/P, JASON, ENVISAT), and TECs from GPS-LEO occultation systems (e.g., FORMOSAT-3/COSMIC, CHAMP) with heterogeneous sampling and accuracy. 相似文献
63.
Stefano Ettori Annamaria Donnarumma Etienne Pointecouteau Thomas H. Reiprich Stefania Giodini Lorenzo Lovisari Robert W. Schmidt 《Space Science Reviews》2013,177(1-4):119-154
We review the methods adopted to reconstruct the mass profiles in X-ray luminous galaxy clusters. We discuss the limitations and the biases affecting these measurements and how these mass profiles can be used as cosmological proxies. 相似文献
64.
Leblanc F. Schmidt C. Mangano V. Mura A. Cremonese G. Raines J. M. Jasinski J. M. Sarantos M. Milillo A. Killen R. M. Massetti S. Cassidy T. Vervack R. J. Kameda S. Capria M. T. Horanyi M. Janches D. Berezhnoy A. Christou A. Hirai T. Lierle P. Morgenthaler J. 《Space Science Reviews》2022,218(1):1-22
Space Science Reviews - As a hyperspectral imager aboard the orbiter “HX-1” of China’s first Mars mission, the Mars Mineralogical Spectrometer (MMS) is designed with hyperspectral... 相似文献
65.
Future space systems, such as Columbus, the planned European contribution to the International Space Station, offer ample possibilities for microgravity research and application. These new opportunities require adequate user support on ground and novel operational concepts in order to ensure an effective utilization. Extensive experience in microgravity user support has been accumulated at DFVLR during the past Spacelab 1 and D1 missions. Based on this work, a Microgravity User Support Centre (MUSC) has been built and is active for the forthcoming EURECA-A1 and D2 missions, to form an integrated support centre for the disciplines life sciences and material sciences in the Space Station era. The objective of the user support at MUSC is to achieve:
- • easy access to space experiments for scientific and commercial users,
- • efficient preparation of experiments,
- • optimum use of valuable microgravity experimentation time,
- • cost reduction by concentration of experience.