Construction of Temperature Climate Data Records in the Upper Troposphere and Lower Stratosphere Using Multiple RO Missions From September 2006 to July 2023 at NESDIS/STAR

Jun Zhou,Shu-peng Ho,Xinjia Zhou,Xi Shao,Guojun Gu,Yong Chen,Tung-Chang Liu,Xin Jing

Published 2025 in Journal of Geophysical Research: Atmospheres

ABSTRACT

We develop a new monthly zonal mean climatology (MMC) in the upper troposphere and lower stratosphere from September 2006 to July 2023 using the dry temperature profiles from multiple global navigation satellite system (GNSS) radio occultation (RO) missions processed by the GNSS RO Science and Data Center (SDC) at the NOAA Center for Satellite Applications and Research (STAR). The multiple RO missions include Formosa Satellite Mission 3/Constellation Observing System for Meteorology, Ionosphere, and Climate (COSMIC‐1), SPIRE, and Meteorological Operational satellite (MetOp)‐A, ‐B, ‐C. We compare collocated profiles from multiple STAR‐processed RO missions to ensure the consistency of the data used in the construction of STAR MMC. Because the Constellation Observing System for Meteorology, Ionosphere, and Climate‐2 (COSMIC‐2) contains a noticeable temperature difference compared with other RO missions, we decided not to include it. We validate the robustness of the sampling error correction method through three reanalyses: ERA‐5, MERRA‐2, and JRA‐55. The result shows the uncertainty caused by using different reanalyses is negligible. This STAR MMC is then compared with the ROM SAF MMC and the MMC derived from these three reanalyses, exhibiting general consistency. Various climate signals, including quasi‐biennial oscillation (QBO) and El Niño–Southern Oscillation (ENSO), can be identified from STAR MMC. The global temperature trends from STAR MMC show a prominent warming of 0.310 ± 0.128 K/Decade in the upper troposphere and a robust cooling of −0.295 ± 0.145 K/Decade in the mid‐stratosphere. These results demonstrate that STAR MMC can capture climate signals and monitor long‐term climate change.

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