Neural Networks for Arctic Atmosphere Sounding From Radio Occultation Data

被引:13
|
作者
Pelliccia, Fabrizio [1 ]
Pacifici, Fabio [2 ]
Bonafoni, Stefania [1 ]
Basili, Patrizia [1 ]
Pierdicca, Nazzareno [3 ]
Ciotti, Piero [4 ,5 ]
Emery, William J. [6 ]
机构
[1] Univ Perugia, Elect & Informat Engn Dept, I-06125 Perugia, Italy
[2] Univ Roma Tor Vergata, Dept Informat Syst & Prod, I-00133 Rome, Italy
[3] Sapienza Univ Rome, Dept Elect Engn, I-00184 Rome, Italy
[4] Univ Aquila, Elect & Informat Engn Dept, I-67040 Poggio Di Roio, AQ, Italy
[5] Univ Aquila, Ctr Excellence CETEMPS, I-67040 Poggio Di Roio, AQ, Italy
[6] Univ Colorado, Boulder, CO 80309 USA
来源
关键词
Global models; Global Positioning System (GPS); neural network (NN); radio occultation (RO); troposphere; WATER-VAPOR; LAND-COVER; PROFILES; CLASSIFICATION; ASSIMILATION; TEMPERATURE; RETRIEVAL; INVERSION; SAR;
D O I
10.1109/TGRS.2011.2153859
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
This paper illustrates a procedure for the retrieval of tropospheric profiles (temperature, pressure, and humidity) using only refractivity profiles coming from Global Positioning System (GPS)-low-Earth-orbit radio occultation, without the constraint of independent knowledge of atmospheric parameters at each GPS occultation. In order to achieve this goal, we have used an approach based on neural networks (NNs), exploiting a data set of 1106 occultations collected over the Arctic region during the winter season of 2007 and 2008. Total refractivity (N) profiles from Formosa Satellite 3 (FORMOSAT-3)/Constellation Observing System for Meteorology Ionosphere and Climate (COSMIC) satellites have been used as input for training the NNs, whereas the target profiles of dry and wet components (N-d and N-w) were derived using prior information on dry and wet fractions of the total refractivity provided by the analysis of the European Centre for Medium-RangeWeather Forecast (ECMWF). Once we have retrieved N-d and N-w by the trained networks, the other atmospheric parameters (pressure, temperature, and vapor) can be computed, and we have done so relative to colocated ECMWF data, which we have assumed as atmospheric truth. Finally, some comparisons with radiosonde observations (RAOBs) are shown, and performances and potential of the proposed approach are discussed. Profiles computed using 1-D variational retrieval by the COSMIC Data Analysis and Archive Center have also been considered as a benchmark in the RAOB comparison.
引用
收藏
页码:4846 / 4855
页数:10
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