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Assimilation experiments with CHAMP GPS radio occultation measurements
Author(s) -
Healy S. B.,
Thépaut J.N.
Publication year - 2006
Publication title -
quarterly journal of the royal meteorological society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.744
H-Index - 143
eISSN - 1477-870X
pISSN - 0035-9009
DOI - 10.1256/qj.04.182
Subject(s) - radiosonde , radio occultation , geopotential height , geopotential , environmental science , data assimilation , troposphere , meteorology , stratosphere , global positioning system , surface pressure , zenith , remote sensing , atmospheric sciences , geodesy , geology , physics , computer science , precipitation , telecommunications
Abstract A one‐dimensional bending‐angle observation operator for assimilating GPS radio occultation (RO) measurements has been integrated into the ECMWF four‐dimensional variational assimilation (4D‐Var) system. We have performed forecast impact experiments with 60 days of CHAMP RO measurements, in addition to the latest set of conventional and satellite data that are assimilated operationally, including radiances from the Atmospheric Infrared Sounder. It is demonstrated that the CHAMP measurements provide extremely good temperature information in the upper troposphere and lower stratosphere. In the southern hemisphere (SH), they produce a clear, statistically significant improvement in the r.m.s. forecast fit to radiosonde measurements over the day 1 to day 5 forecast range at 300, 200, 100 and 50 hPa. An improved r.m.s. fit to radiosondes is also evident at 100 hPa in the tropics. However, the observations degrade the 500 hPa geopotential height (500Z) field in the SH. This appears to be mainly caused by erroneous surface pressure increments in Antarctica. As a result, we have modified the GPS tangent‐linear and adjoint routines, prior to the evaluation of the model‐level pressures and geopotential heights, in order to remove the sensitivity of the model geopotential height values to the surface pressure. This improves the SH 500Z forecast scores, although a small degradation is still evident at the day 1 and day 2 forecast range. A simple method for estimating the degrees of freedom for signal (DFS) of a large variational assimilation system is noted and applied to estimate the DFS of the CHAMP measurements assimilated during a 12‐hour assimilation window. The CHAMP measurements increase the total DFS of the 4D‐Var system by ∼4%, and the DFS per CHAMP bending‐angle profile is ∼34. Copyright © 2006 Royal Meteorological Society