Initial Assessment of the COSMIC-2/FORMOSAT-7 Neutral Atmosphere Data Quality in NESDIS/STAR Using In Situ and Satellite Data

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...

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Main Authors: Shu-Peng Ho, Xinjia Zhou, Xi Shao, Bin Zhang, Loknath Adhikari, Stanislav Kireev, Yuxiang He, James G. Yoe, Wei Xia-Serafino, Erin Lynch
Format: Article
Language:English
Published: MDPI AG 2020-12-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/12/24/4099
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author Shu-Peng Ho
Xinjia Zhou
Xi Shao
Bin Zhang
Loknath Adhikari
Stanislav Kireev
Yuxiang He
James G. Yoe
Wei Xia-Serafino
Erin Lynch
author_facet Shu-Peng Ho
Xinjia Zhou
Xi Shao
Bin Zhang
Loknath Adhikari
Stanislav Kireev
Yuxiang He
James G. Yoe
Wei Xia-Serafino
Erin Lynch
author_sort Shu-Peng Ho
collection DOAJ
description 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 <i>v/v</i> to about 2800 <i>v/v</i>. 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 <i>v/v</i> group, 500–1000 <i>v/v</i> group, 1000–1500 <i>v/v</i> group, 1500–2000 <i>v/v</i> group, and >2000 <i>v/v</i> 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 <i>v/v</i>), −1.17 g/kg (500–1000 <i>v/v</i>), −1.33 g/kg (1000–1500 <i>v/v</i>), −0.93 g/kg (1500–2000 <i>v/v</i>), and −1.52 g/kg (>2000 <i>v/v</i>). Except for the >2000 <i>v/v</i> 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 <i>v/v</i> group) comparing with those from lower SNR groups.
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spelling doaj.art-dd230c01aa414bb4bda23feddf69a60b2023-11-21T00:56:54ZengMDPI AGRemote Sensing2072-42922020-12-011224409910.3390/rs12244099Initial Assessment of the COSMIC-2/FORMOSAT-7 Neutral Atmosphere Data Quality in NESDIS/STAR Using In Situ and Satellite DataShu-Peng Ho0Xinjia Zhou1Xi Shao2Bin Zhang3Loknath Adhikari4Stanislav Kireev5Yuxiang He6James G. Yoe7Wei Xia-Serafino8Erin Lynch9Center for Satellite Applications & Research (STAR), NESDIS/NOAA, College Park, MD 20740, USAGlobal Science & Technology, Inc., 7855 Walker Drive, Suite 200, Greenbelt, MD 20770, USACooperative Institute for Satellite Earth System Studies (CISESS), Earth System Science, Interdisciplinary Center, University of Maryland, College Park, MD 20740, USACooperative Institute for Satellite Earth System Studies (CISESS), Earth System Science, Interdisciplinary Center, University of Maryland, College Park, MD 20740, USACooperative Institute for Satellite Earth System Studies (CISESS), Earth System Science, Interdisciplinary Center, University of Maryland, College Park, MD 20740, USAGlobal Science & Technology, Inc., 7855 Walker Drive, Suite 200, Greenbelt, MD 20770, USAGlobal Science & Technology, Inc., 7855 Walker Drive, Suite 200, Greenbelt, MD 20770, USANational Weather Service, National Centers for Environmental Prediction (NCEP), NOAA, 1325 East West Highway, Silver Spring, MD 20910, USAOffice of Project, Planning, and Analysis, NOAA, Suite 6200 (6th Floor), 1335 East West Highway, Silver Spring, MD 20910, USACooperative Institute for Satellite Earth System Studies (CISESS), Earth System Science, Interdisciplinary Center, University of Maryland, College Park, MD 20740, USAA 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 <i>v/v</i> to about 2800 <i>v/v</i>. 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 <i>v/v</i> group, 500–1000 <i>v/v</i> group, 1000–1500 <i>v/v</i> group, 1500–2000 <i>v/v</i> group, and >2000 <i>v/v</i> 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 <i>v/v</i>), −1.17 g/kg (500–1000 <i>v/v</i>), −1.33 g/kg (1000–1500 <i>v/v</i>), −0.93 g/kg (1500–2000 <i>v/v</i>), and −1.52 g/kg (>2000 <i>v/v</i>). Except for the >2000 <i>v/v</i> 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 <i>v/v</i> group) comparing with those from lower SNR groups.https://www.mdpi.com/2072-4292/12/24/4099GPS ROCOSMIC-2neutral atmospheric profilessatellite and in situ radiosonde observationslong term stabilityaccuracy
spellingShingle Shu-Peng Ho
Xinjia Zhou
Xi Shao
Bin Zhang
Loknath Adhikari
Stanislav Kireev
Yuxiang He
James G. Yoe
Wei Xia-Serafino
Erin Lynch
Initial Assessment of the COSMIC-2/FORMOSAT-7 Neutral Atmosphere Data Quality in NESDIS/STAR Using In Situ and Satellite Data
Remote Sensing
GPS RO
COSMIC-2
neutral atmospheric profiles
satellite and in situ radiosonde observations
long term stability
accuracy
title Initial Assessment of the COSMIC-2/FORMOSAT-7 Neutral Atmosphere Data Quality in NESDIS/STAR Using In Situ and Satellite Data
title_full Initial Assessment of the COSMIC-2/FORMOSAT-7 Neutral Atmosphere Data Quality in NESDIS/STAR Using In Situ and Satellite Data
title_fullStr Initial Assessment of the COSMIC-2/FORMOSAT-7 Neutral Atmosphere Data Quality in NESDIS/STAR Using In Situ and Satellite Data
title_full_unstemmed Initial Assessment of the COSMIC-2/FORMOSAT-7 Neutral Atmosphere Data Quality in NESDIS/STAR Using In Situ and Satellite Data
title_short Initial Assessment of the COSMIC-2/FORMOSAT-7 Neutral Atmosphere Data Quality in NESDIS/STAR Using In Situ and Satellite Data
title_sort initial assessment of the cosmic 2 formosat 7 neutral atmosphere data quality in nesdis star using in situ and satellite data
topic GPS RO
COSMIC-2
neutral atmospheric profiles
satellite and in situ radiosonde observations
long term stability
accuracy
url https://www.mdpi.com/2072-4292/12/24/4099
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