Validation of the COSMIC Radio Occultation Data over Gadanki (13.48°N, 79.2°E): A Tropical Region

Constellation Observing System for Meteorology Ionosphere and Climate (COSMIC), consisting of six Low Earth Orbit (LEO) Global Position System (GPS) receivers, on board the Formosat Satellite 3 (FORMOSAT-3) is providing dense observations of density, refractivity, temperature and water vapor profile...

Full description

Bibliographic Details
Main Authors: D. Narayana Rao, M. Venkat Ratnam, Sanjay Mehta, Debashis Nath, S. Ghouse Basha, V. V. M. Jagannadha Rao, B. V. Krishna Murthy, T. Tsuda, Kenji Nakamura
Format: Article
Language:English
Published: Springer 2009-01-01
Series:Terrestrial, Atmospheric and Oceanic Sciences
Subjects:
Online Access: http://tao.cgu.org.tw/images/attachments/v201p059.pdf
_version_ 1818139476526891008
author D. Narayana Rao
M. Venkat Ratnam
Sanjay Mehta
Debashis Nath
S. Ghouse Basha
V. V. M. Jagannadha Rao
B. V. Krishna Murthy
T. Tsuda
Kenji Nakamura
author_facet D. Narayana Rao
M. Venkat Ratnam
Sanjay Mehta
Debashis Nath
S. Ghouse Basha
V. V. M. Jagannadha Rao
B. V. Krishna Murthy
T. Tsuda
Kenji Nakamura
author_sort D. Narayana Rao
collection DOAJ
description Constellation Observing System for Meteorology Ionosphere and Climate (COSMIC), consisting of six Low Earth Orbit (LEO) Global Position System (GPS) receivers, on board the Formosat Satellite 3 (FORMOSAT-3) is providing dense observations of density, refractivity, temperature and water vapor profiles of the neutral atmosphere since middle of July 2006. Special radiosonde (Väisälä) campaign was conducted at Gadanki (13.48°N, 79.18°E), a tropical site in India, during July 2006 to March 2007 to validate these meteorological parameters. Co-located Nd: YAG Rayleigh lidar was also operated during the overpass of COSMIC and is utilized to validate the temperatures in the height range of 30 to 40 km. Atotal of 142 overpasses occurred during the above mentioned period within 300 km distance from Gadanki out of which 41 overpasses occurred within a time difference of ±4 hours of radiosonde launch. In addition, 18 overpasses occurred within the time difference of ±4 hours of lidar operation. A detailed comparison has been made with all these overpasses for the refractivity, temperature and water vapor obtained from COSMIC. The water vapor comparison has shown generally a good agreement with a mean difference of 5 - 10% below 6 - 7 km. Although there is a colder bias between COSMIC and radiosonde, a very good comparison in temperature is also found between 10 and 27 km with a mean difference of less than 1 K (RMS difference is only 0.64 K). There exists a large difference in temperature of about 8 K between 30 and 40 km (between COSMIC and lidar). Possible reasons for these large differences are given. There was one event that occurred just over Gadanki for which a detailed comparison has been made with special emphasis on water vapor retrievals. Sensitivity test is also done on the fractional difference in N for the event that occurred on 24 July 2006 between COSMIC (1D-var) and radiosonde and found that pressure plays a key role than temperature in determining the refractivity.
first_indexed 2024-12-11T10:28:42Z
format Article
id doaj.art-92c48ff31c574be7a3b661486e6f18a3
institution Directory Open Access Journal
issn 1017-0839
2311-7680
language English
last_indexed 2024-12-11T10:28:42Z
publishDate 2009-01-01
publisher Springer
record_format Article
series Terrestrial, Atmospheric and Oceanic Sciences
spelling doaj.art-92c48ff31c574be7a3b661486e6f18a32022-12-22T01:11:03ZengSpringerTerrestrial, Atmospheric and Oceanic Sciences1017-08392311-76802009-01-0120105910.3319/TAO.2008.01.23.01(F3C)814Validation of the COSMIC Radio Occultation Data over Gadanki (13.48°N, 79.2°E): A Tropical RegionD. Narayana RaoM. Venkat RatnamSanjay MehtaDebashis NathS. Ghouse BashaV. V. M. Jagannadha RaoB. V. Krishna MurthyT. TsudaKenji NakamuraConstellation Observing System for Meteorology Ionosphere and Climate (COSMIC), consisting of six Low Earth Orbit (LEO) Global Position System (GPS) receivers, on board the Formosat Satellite 3 (FORMOSAT-3) is providing dense observations of density, refractivity, temperature and water vapor profiles of the neutral atmosphere since middle of July 2006. Special radiosonde (Väisälä) campaign was conducted at Gadanki (13.48°N, 79.18°E), a tropical site in India, during July 2006 to March 2007 to validate these meteorological parameters. Co-located Nd: YAG Rayleigh lidar was also operated during the overpass of COSMIC and is utilized to validate the temperatures in the height range of 30 to 40 km. Atotal of 142 overpasses occurred during the above mentioned period within 300 km distance from Gadanki out of which 41 overpasses occurred within a time difference of ±4 hours of radiosonde launch. In addition, 18 overpasses occurred within the time difference of ±4 hours of lidar operation. A detailed comparison has been made with all these overpasses for the refractivity, temperature and water vapor obtained from COSMIC. The water vapor comparison has shown generally a good agreement with a mean difference of 5 - 10% below 6 - 7 km. Although there is a colder bias between COSMIC and radiosonde, a very good comparison in temperature is also found between 10 and 27 km with a mean difference of less than 1 K (RMS difference is only 0.64 K). There exists a large difference in temperature of about 8 K between 30 and 40 km (between COSMIC and lidar). Possible reasons for these large differences are given. There was one event that occurred just over Gadanki for which a detailed comparison has been made with special emphasis on water vapor retrievals. Sensitivity test is also done on the fractional difference in N for the event that occurred on 24 July 2006 between COSMIC (1D-var) and radiosonde and found that pressure plays a key role than temperature in determining the refractivity. http://tao.cgu.org.tw/images/attachments/v201p059.pdf GPS ROWater vaporTemperatureValidation
spellingShingle D. Narayana Rao
M. Venkat Ratnam
Sanjay Mehta
Debashis Nath
S. Ghouse Basha
V. V. M. Jagannadha Rao
B. V. Krishna Murthy
T. Tsuda
Kenji Nakamura
Validation of the COSMIC Radio Occultation Data over Gadanki (13.48°N, 79.2°E): A Tropical Region
Terrestrial, Atmospheric and Oceanic Sciences
GPS RO
Water vapor
Temperature
Validation
title Validation of the COSMIC Radio Occultation Data over Gadanki (13.48°N, 79.2°E): A Tropical Region
title_full Validation of the COSMIC Radio Occultation Data over Gadanki (13.48°N, 79.2°E): A Tropical Region
title_fullStr Validation of the COSMIC Radio Occultation Data over Gadanki (13.48°N, 79.2°E): A Tropical Region
title_full_unstemmed Validation of the COSMIC Radio Occultation Data over Gadanki (13.48°N, 79.2°E): A Tropical Region
title_short Validation of the COSMIC Radio Occultation Data over Gadanki (13.48°N, 79.2°E): A Tropical Region
title_sort validation of the cosmic radio occultation data over gadanki 13 48°n 79 2°e a tropical region
topic GPS RO
Water vapor
Temperature
Validation
url http://tao.cgu.org.tw/images/attachments/v201p059.pdf
work_keys_str_mv AT dnarayanarao validationofthecosmicradiooccultationdataovergadanki1348n792eatropicalregion
AT mvenkatratnam validationofthecosmicradiooccultationdataovergadanki1348n792eatropicalregion
AT sanjaymehta validationofthecosmicradiooccultationdataovergadanki1348n792eatropicalregion
AT debashisnath validationofthecosmicradiooccultationdataovergadanki1348n792eatropicalregion
AT sghousebasha validationofthecosmicradiooccultationdataovergadanki1348n792eatropicalregion
AT vvmjagannadharao validationofthecosmicradiooccultationdataovergadanki1348n792eatropicalregion
AT bvkrishnamurthy validationofthecosmicradiooccultationdataovergadanki1348n792eatropicalregion
AT ttsuda validationofthecosmicradiooccultationdataovergadanki1348n792eatropicalregion
AT kenjinakamura validationofthecosmicradiooccultationdataovergadanki1348n792eatropicalregion