Abstract
A COSMIC-1/FORMOSAT-3 (Constellation Observing System for Meteorology, Ionosphere, and Climate-1 and Formosa Satellite Mission 3) follow-on mission, COSMIC-2/FORMOSAT-7, had been successfully launched into low-inclination orbits on 25 June 2019. COSMIC-2 has a significantly increased Signal-to-Noise ratio (SNR) compared to other Radio Occultation (RO) missions. This study summarized the initial assessment of COSMIC-2 data quality conducted by the NOAA (National Oceanic and Atmospheric Administration) Center for Satellite Applications and Research (STAR). We use validated data from other RO missions to quantify the stability of COSMIC-2. In addition, we use the Vaisala RS41 radiosonde observations to assess the accuracy and uncertainty of the COSMIC-2 neutral atmospheric profiles. RS41 is currently the most accurate radiosonde observation system. The COSMIC-2 SNR ranges from 200 v/v to about 2800 v/v. To see if the high SNR COSMIC-2 signals lead to better retrieval results, we separate the COSMIC-2–RS41 comparisons into different SNR groups (i.e., 0–500 v/v group, 500–1000 v/v group, 1000–1500 v/v group, 1500–2000 v/v group, and >2000 v/v group). In general, the COSMIC-2 data quality in terms of stability, precision, accuracy, and uncertainty of the accuracy is very compatible with those from COSMIC-1. Results show that the mean COSMIC-2–RS41 water vapor difference from surface to 5 km altitude for each SNR groups are equal to −1.34 g/kg (0–500 v/v), −1.17 g/kg (500–1000 v/v), −1.33 g/kg (1000–1500 v/v), −0.93 g/kg (1500–2000 v/v), and −1.52 g/kg (>2000 v/v). Except for the >2000 v/v group, the high SNR measurements from COSMIC-2 seem to improve the mean water vapor difference for the higher SNR group slightly (especially for the 1500–2000 v/v group) comparing with those from lower SNR groups.
Highlights
Since its launch in 2006, the Constellation Observing System for Meteorology, Ionosphere, and Climate (COSMIC) 1 mission and Formosa Satellite Mission 3 (COSMIC-1/FORMOSAT-3, hereafter COSMIC-1) has provided more than 7.0 million global neutral atmospheric profiles in the lower stratosphere and troposphere [1]
Using the Global Positioning System (GPS) radio occultation (RO) technique, COSMIC data are of all-weather capability and high vertical resolution (~200–600 m, [2])
Studies have demonstrated that the high vertical resolution COSMIC-1 neutral atmospheric profiles, which are not very sensitive to clouds and precipitation [3], are very useful for studying atmospheric processes [4,5,6,7]
Summary
Since its launch in 2006, the Constellation Observing System for Meteorology, Ionosphere, and Climate (COSMIC) 1 mission and Formosa Satellite Mission 3 (COSMIC-1/FORMOSAT-3, hereafter COSMIC-1) has provided more than 7.0 million (as of the middle of 2019) global neutral atmospheric profiles in the lower stratosphere and troposphere [1]. UCAR CDAAC has adapted the COSMIC data processing package to convert the COSMIC-2 phase delay into vertical profiles of bending angle, refractivity, temperature, and moisture. This COSMIC processing package has been used to process COSMIC data and RO data from Challenging Minisatellite Payload, Korea Multi-Purpose Satellite-5 (KOMPSAT-5), and Meteorological Operational Series (i.e., MetOp-A, -B, -C) Receiver for Atmospheric Sounding (GRAS). We used neutral atmospheric variables derived from multiple RO missions, including COSMIC, KOMPSAT-5, and MetOp-A GRAS, and TSX, processed by CDAAC, to validate the stability of COSMIC-2. The data quality of these RO missions (except for COSMIC-2), including precision, stability, and structural uncertainty owing to inversion implementations, has been intensively validated in previous studies (i.e., [30,31,32]). We used data from multiple RO missions from October 2019 to January 2020 to quantify the stability of COSMIC-2 observations
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