JpGU-AGU Joint Meeting 2017

講演情報

[JJ] 口頭発表

セッション記号 A (大気水圏科学) » A-OS 海洋科学・海洋環境

[A-OS22] [JJ] 海洋物理学

2017年5月22日(月) 09:00 〜 10:30 302 (国際会議場 3F)

コンビーナ:東塚 知己(東京大学大学院理学系研究科地球惑星科学専攻)、吉川 裕(京都大学大学院理学研究科)、Shinya Kouketsu(JAMSTEC Japan Agency for Marine-Earth Science and Technology)、田中 祐希(東京大学大学院理学系研究科)、座長:東塚 知己(東京大学大学院理学系研究科地球惑星科学専攻)、座長:纐纈 慎也(JAMSTEC)

09:15 〜 09:30

[AOS22-02] Long-term change and variation of salinity in the western North Pacific subtropical gyre revealed by 50-year long observations along 137ºE

★招待講演

*岡 英太郎1桂 将太1井上 博敬2小嶋 惇2,3北本 萌子2,3中野 俊也2,3須賀 利雄4,5 (1.東京大学大気海洋研究所、2.気象庁地球環境・海洋部、3.気象研究所海洋・地球化学研究部、4.東北大学理学研究科、5.海洋研究開発機構地球環境観測研究開発センター)

キーワード:Western North Pacific subtropical gyre, Main thermocline/halocline, Long-term change, Decadal variability, Repeat hydrographic section

The 137ºE repeat hydrographic section for 50 winters during 1967−2016 has been analyzed to examine interannual to interdecadal variations and long-term changes of salinity and temperature in the surface and intermediate layers of the western North Pacific, with a particular focus on freshening in the subtropical gyre. Rapid freshening on both isobars and isopycnals began in mid-1990’s and persisted for the last 20 years in the upper main thermocline/halocline in the western subtropical gyre. In addition, significant decadal variability of salinity existed in the Subtropical Mode Water (STMW), as previously reported for the shallower layers. An analysis of the 144ºE repeat hydrographic section during 1984−2013 supplemented by Argo profiling float data in 2014 and 2015 revealed that the freshening trend and decadal variability observed at 137ºE originated in the winter mixed layer in the Kuroshio Extension (KE) region and was transmitted southwestward to 137ºE 1−2 years later in association with the subduction and advection of STMW. The mechanism of these changes and variations in the source region was further investigated. In addition to the surface freshwater flux in the KE region pointed out by previous studies, the decadal KE variability in association with the Pacific Decadal Oscillation likely contributes to the decadal salinity variability through water exchange between the subtropics and the subarctic across the KE. Interdecadal change in both the surface freshwater flux and the KE state, however, failed to explain the rapid freshening for the last 20 years.