"Ocean mixed layer variation by MJOs during Pre-YMC2015 & YMC2017" Moteki MSJ Spring 180517 @ Tsukuba
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"Ocean mixed layer variation by MJOs during Pre-YMC2015 & YMC2017" Moteki MSJ Spring 180517 @ Tsukuba
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"Ocean mixed layer variation by MJOs during Pre-YMC2015 & YMC2017" Moteki MSJ Spring 180517 @ Tsukuba
- 3. passed over Mirai on 12/13 passed over 1 week before YMC2017Pre-YMC2015 R/V Mirai location / MJO phase
- 4. YMC2017 MR1708 Pre-YMC2015 MR1504 before MJO after MJO weak easterly winds<5m/s SST>30℃ strong westerly winds>10m/s SST<29℃ ocean mixed layer depth <->SST->CAPE/CIN
- 5. YMC2017Pre-YMC2015 before MJO after MJO high SST cooled SST ECCO2-SST : JRA55-Usfc
- 6. YMC2017Pre-YMC2015 before MJO after MJO high SST week easterly cooled SST strong westerly MJ O MJ O MJ O ECCO2-SST : JRA55-Usfc
- 7. YMC2017Pre-YMC2015 before MJO after MJO 24h running mean shallow ML/IL thin BL deep IL fluctuating ML/BL
- 8. YMC2017Pre-YMC2015 before MJO after MJO high SST well mixed T T10m-depth: SST+1〜2℃ T inversion
- 9. YMC2017Pre-YMC2015 before MJO after MJO smaller heat loss larger LHF(〜✖3)
- 10. YMC2017Pre-YMC2015 before MJO after MJO CAPE(1268 J/kg) LCL(948 hPa) CAPE(612 J/kg) LCL(930 hPa)
- 11. YMC2017Pre-YMC2015 before MJO after MJO CIN(-11) LFC(895) CIN(-20) LCL(863)
- 12. YMC2017Pre-YMC2015 before MJO after MJO strong salinity stratification mixed in IL
- 13. YMC2017Pre-YMC2015 before MJO after MJO phytoplankton going down slowly frequent up-down
- 14. YMC2017Pre-YMC2015 before MJO after MJO 1 cast / day shallow ML/IL thin BL more turbulent 8casts daily mean
- 15. YMC2017Pre-YMC2015 before MJO after MJO slow current variable current
- 16. YMC2017Pre-YMC2015 before MJO after MJO southward flow rotational flow
- 17. YMC2017Pre-YMC2015 before MJO after MJO alongshore flow alongshore eddies
- 18. YMC2017 MR1708 Pre-YMC2015 MR1504 before MJO after MJO higher T lower S shallow ML more calm lower T higher S fluctuating ML more turbulent 1.5℃ 2psu 80m 10-2
- 19. YMC2017 MR1708 Pre-YMC2015 MR1504 before MJO after MJO lower LCL large CAPE small CIN well mixed alongshore flow higher LCL small CAPE large CIN T inversion alongshore eddies 18hPa ×2 1/2 surface
- 20. YMC2017Pre-YMC2015 after MJO before MJO alongshore eddies alongshore flow
- 21. YMC2017Pre-YMC2015 before MJO after MJO thin BLT: shallow IL thick BLT: deep IL ECCO2-BLT, ocean current [45-155m]
- 22. YMC2017Pre-YMC2015 before MJO after MJO oceanic downwelling Kelvin wave oceanic Kelvin waves MJ O MJ O MJ O ECCO2-SLA : JRA55-Usfc
- 23. YMC2017Pre-YMC2015 before MJO after MJO shallow ML/IL thin BL deep IL fluctuating ML/BL
- 26. YMC2017Pre-YMC2015 before MJO after MJO slow current variable current S N S N S N
- 27. YMC2017Pre-YMC2015 before MJO after MJO slow current variable current S N S N S N
- 30. 観測 ECCO2 OFES2 ref. dep. = 12.5mref. dep. = 15mref. dep. = 10m 塩分過小〜0.2psu 水温過大〜0.2K 塩分過大〜2psu 水温過小〜1K
- 33. ARGO
- 34. ARGO
- 35. ARGO
Notes de l'éditeur
- 世界的にもJAMSTEC以外ではできない取り組み
- JAMSTECの中期計画では日本の気候変動にMJOが直接影響することをYMCで明らかにする位置づけ
- それを示す非常に貴重なデータを得ることができました．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- では，今日，僕から提供させて頂く話題は，「海と空のあいだに 今日もつゆの雨が降る」、というタイトルです． 今日みなさんに最も分かって頂きたいことは，天気予報を良くするために海洋観測が如何に重要か，両者の関わりは非常に大きい，ということです． 特に，僕は梅雨前線の研究を一番長くやってきているので，梅雨にまつわる海と空との関係についてお話したいと思います．
- このように，みらいの観測海域をMJOが通過するところでデータを得る
- それを示す非常に貴重なデータを得ることができました．
- それを示す非常に貴重なデータを得ることができました．
- それを示す非常に貴重なデータを得ることができました．
- それを示す非常に貴重なデータを得ることができました．
- それを示す非常に貴重なデータを得ることができました．
- それを示す非常に貴重なデータを得ることができました．
- このように，みらいの観測海域をMJOが通過するところでデータを得る
- このように，みらいの観測海域をMJOが通過するところでデータを得る
- それを示す非常に貴重なデータを得ることができました．
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to
- like this. This is a time-depth cross section of temperature from 3-hourly CTD observation. Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line. The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December. Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m. Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m. Then, BLT is drastically deepening during the MJO passage. This time lag of deepening of ILD and MLD is due to