日本地球惑星科学連合2025年大会

講演情報

[E] 口頭発表

セッション記号 A (大気水圏科学) » A-AS 大気科学・気象学・大気環境

[A-AS06] 大気圏(成層圏・対流圏)過程とその気候への影響

2025年5月27日(火) 10:45 〜 12:15 105 (幕張メッセ国際会議場)

コンビーナ:野口 峻佑(九州大学 理学研究院 地球惑星科学部門)、原田 やよい(気象研究所)、西井 和晃(三重大学大学院生物資源学研究科)、江口 菜穂(九州大学 応用力学研究所)、座長:西井 和晃(三重大学大学院生物資源学研究科)、江口 菜穂(九州大学 応用力学研究所)



11:30 〜 11:45

[AAS06-09] 20 Years of Atmospheric Temperature, Water Vapor, and Cloud Products Derived from Multiple Satellite Hyperspectral Remote Sensors

*Xu Liu1 (1.NASA Langley Research Center)

キーワード:stratospheric intrusion, climate change, temperature trend, water vapor trend

Deriving Climate Data Records (CDRs) from multiple IR sounders such AIRS on Aqua, CrIS on S-NPP, NOAA20 and JPSS-2, IASI on Metop A, B, and C from current operational products faces several challenges. First it is a time-consuming process to generate level-2 data products since modern hyperspectral satellite sensors have millions of observations each day with thousands of spectral channels for each observation. Additionally, differences in radiative transfer models and retrieval algorithms used to process level 2 data can lead to errors in the climate products when fusing data from different satellite sensors. We have developed a Climate Fingerprinting Sounder Product (ClimFiSP) algorithm, which uses a single set of radiative kernels and a robust spectral fingerprinting method to perform retrievals using spatiotemporally averaged L1 hyperspectral radiances directly. The ClimFiSP algorithm provides accurate data fusion CDR products from multiple satellite sensors. We have applied this method to both AIRS and CrIS (on SNPP and on NOAA 20) data and generated two decades climate data records at 0.5 by 0.5 degree grid on global scale. We plan to add IASI to the CDR data set in the future. The ClimFiSP CDR products will be released for public access in the first quarter of 2025 at the NASA Goddard Earth Sciences (GES) Data and Information Services Center (DISC). These long-term CDRs include: 1) vertical profiles of atmospheric temperature, water vapor, ozone, and carbon monoxide; 2) height, temperature, particle size, and optical depths for ice and water clouds, and 3) surface skin temperature and surface emissivity spectra.
In this presentation, we will show examples of the polar vortex break up and stratospheric intrusion based on our retrieval results. We will also show long term global trends for both stratosphere and troposphere temperature, water vapor, ozone, and clouds.