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Comparison of three retrievals of COSMIC GPS radio occultation results in the tropical upper troposphere and lower stratosphere

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Comparison of three retrievals of COSMIC GPS radio occultation results in the tropical upper troposphere and lower stratosphere

国立国会図書館請求記号
Z74-F717
国立国会図書館書誌ID
10953853
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info:ndljp/pid/10953853
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記事
著者
Noersomadiほか
出版者
Springer Nature
出版年
2017-09-11
資料形態
紙・デジタル
掲載誌名
EPS : Earth, Planets and Space 69(125)
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要約等:

Combining geometrical optics (GO) and wave optics (WO), the COSMIC data analysis and archive center (CDAAC) retrieved two sets of dry atmosphere tempe...

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デジタル

資料種別
記事
著者・編者
Noersomadi
Toshitaka Tsuda
出版年月日等
2017-09-11
出版年(W3CDTF)
2017-09-11
タイトル(掲載誌)
EPS : Earth, Planets and Space
巻号年月日等(掲載誌)
69(125)
掲載巻
69(125)
ISSN(掲載誌)
1880-5981
ISSN-L(掲載誌)
1343-8832
本文の言語コード
eng
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info:ndljp/pid/10953853
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コレクション(障害者向け資料:レベル1)
コレクション(個別)
国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
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オンライン資料収集制度
受理日(W3CDTF)
2017-09-14T21:01:06+09:00
保存日(W3CDTF)
2017-09-14
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application/pdf
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国立国会図書館 : 国立国会図書館デジタルコレクション

デジタル

要約等
Combining geometrical optics (GO) and wave optics (WO), the COSMIC data analysis and archive center (CDAAC) retrieved two sets of dry atmosphere temperatures (T) from COSMIC GPS radio occultation (GPS-RO), which are called atmPrf2010 and atmPrf2013. In atmPrf2010, the sewing height between WO and GO varies between 10 and 20 km, but is fixed at 20 km for atmPrf2013. The height resolution of the atmPrf2010 depends on the sewing height, while the T profiles by atmPrf2013 are smoothed over 500 m. We also derived T by applying WO throughout the troposphere and the stratosphere up to a 30-km altitude, which is called rishfsi2013. The three retrievals have different characteristics in the height resolution around the tropopause. Therefore, we aim to examine a possible discrepancy in the statistical results of the cold-point tropopause (CPT) and the lapse rate tropopause (LRT) among the three datasets, conducting their inter-comparisons as well as the comparison between GPS-RO and the simultaneous radiosonde dataset. We investigate the T variations in the upper troposphere and lower stratosphere (UTLS) over the tropics from October 1, 2011, to March 31, 2012, when radiosonde soundings were conducted as the CINDY-DYNAMO 2011 campaign. The mean T profiles are consistent between atmPrf2010 and atmPrf2013, but rishfsi2013 results are colder (warmer) than the CDAAC retrievals below (above) the tropopause. The mean T difference between atmPrf2013 and atmPrf2010 is 0.17 K at the cold-point tropopause (CPT) and −0.38 K at the lapse rate tropopause (LRT). On the other hand, rishfsi2013 shows a colder T at CPT by −0.77 and −0.59 K relative to atmPrf2013 and atmPrf2010, respectively, and the warmer T by 0.60 and 0.20 Kd at LRT. During CINDY-DYNAMO, we found 134 radiosonde soundings that coincide with GPS-RO within ±3 h and are collocated within 200 km from GPS-RO. The mean T difference at CPT from the radiosondes is 0.32, 0.49 and −0.24 K for atmPrf2010, atmPrf2013 and rishfsi2013, respectively. Both atmPrf2013 and atmPrf2010 have a positive bias at CPT, while rishfsi2013 has a negative one. Similar comparisons at LRT are −0.45, −0.69 and −0.41 K, respectively, showing a negative bias for all GPS-RO retrievals. The results show that rishfsi2013 is consistent with the retrievals at CDAAC and the radiosondes. Due to its good height resolution, rishfsi2013 is useful for studies on mesoscale T perturbations in the UTLS.
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著作権情報
© The Author(s) 2017. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.
参照
Coordinated Upper-troposphere-to-stratosphere Balloon Experiment in Biak (CUBE/Biak)
Influence of ENSO and MJO on the zonal structure of tropical tropopause inversion layer using high-resolution temperature profiles retrieved from COSMIC GPS Radio Occultation
Tropical Temperature Variability in the UTLS: New Insights from GPS Radio Occultation Observations
参照
Analysis of vertical wave number spectrum of atmospheric gravity waves in the stratosphere using COSMIC GPS radio occultation data
Observing Earth's atmosphere with radio occultation measurements using the Global Positioning System
Quantifying uncertainty in climatological fields from GPS radio occultation: an empirical-analytical error model
Exploring Earth's atmosphere with radio occultation: contributions to weather, climate and space weather
Representativeness errors for radiosonde observations
Optimal Noise Filtering for the Ionospheric Correction of GPS Radio Occultation Signals
Tropical Cold-Point Tropopause: Climatology, Seasonal Cycle, and Intraseasonal Variability Derived from COSMIC GPS Radio Occultation Measurements
Global distribution of atmospheric waves in the equatorial upper troposphere and lower stratosphere: COSMIC observations of wave mean flow interactions
Geometrical optics phase matching of radio occultation signals
Full Spectrum Inversion of radio occultation signals
On the uncertainty of radio occultation inversions in the lower troposphere
Comparing radiosonde and COSMIC atmospheric profile data to quantify differences among radiosonde types and the effects of imperfect collocation on comparison statistics
The occurrence of cirrus clouds associated with eastward propagating equatorial <i>n</i> = 0 inertio‐gravity and Kelvin waves in November 2011 during the CINDY2011/DYNAMO campaign
Cracking the MJO nut
Analysis of wave fields by Fourier integral operators and their application for radio occultations
Assessment of COSMIC radio occultation retrieval product using global radiosonde data
Ionospheric correction of GPS radio occultation data in the troposphere
Comparison of GPS radio occultation soundings with radiosondes
Validation of FORMOSAT-3/COSMIC level 2 "atmPrf" global temperature data in the stratosphere
Tropical tropopause layer
Analysis of GPS radio occultation data from the FORMOSAT-3/COSMIC and Metop/GRAS missions at CDAAC
The COSMIC/FORMOSAT-3 Mission: Early Results
Reconstruction of internal gravity wave parameters from radio occultation retrievals of vertical temperature profiles in the Earth's atmosphere
GPS Sounding of the Atmosphere from Low Earth Orbit: Preliminary Results
Use of the L2C signal for inversions of GPS radio occultation data in the neutral atmosphere
Global multiple tropopause features derived from COSMIC radio occultation data during 2007 to 2012
Tracking Pulses of the Madden–Julian Oscillation
Climate intercomparison of GPS radio occultation, RS90/92 radiosondes and GRUAN from 2002 to 2013
GPS radio occultation for climate monitoring and change detection
THE EXTRATROPICAL UPPER TROPOSPHERE AND LOWER STRATOSPHERE
Canonical transform method for processing radio occultation data in the lower troposphere
On the variability of temperature profiles in the stratosphere: Implications for validation
Tropical temperature variability and Kelvin-wave activity in the UTLS from GPS RO measurements
Inversion and Error Estimation of GPS Radio Occultation Data (3.Application of GPS Data to Atmospheric Science)
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書誌ID(NDLBibID)
10953853
NII論文ID
120006364091