Journal of Tropical Oceanography ›› 2024, Vol. 43 ›› Issue (5): 17-31.doi: 10.11978/2023141CSTR: 32234.14.2023141
• Marine Meteorology • Previous Articles Next Articles
SUN Zeming1(), HAN Shuzong1,2(
), WANG Mingjie1, SU Hanxiang1
Received:
2023-10-04
Revised:
2023-12-07
Online:
2024-09-10
Published:
2024-10-10
Supported by:
SUN Zeming, HAN Shuzong, WANG Mingjie, SU Hanxiang. Statistical study on the influence of typhoon with different path on the temperature of coastal waters of China[J].Journal of Tropical Oceanography, 2024, 43(5): 17-31.
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Tab. 1
Spatiotemporal ranges of two optimal interpolated sea surface temperature data sets and corresponding sensors used"
传感器 | 空间范围 | 时间范围 | |
---|---|---|---|
MW | TMI, AMSR-E, AMSR2, WindSat, GMI | 在2002-06-01之前: 40°S—40°N 在2002-06-01之后: 全球 | 1998-01-01 至今 |
MW_IR | MW: TMI, AMSR-E, AMSR2,WindSat, GMI IR: MODIS-Terra, MODIS-Aqua, VIIRS-NPP, VIIRS-N20 | 全球 | 2002-06-01 至今 |
Fig. 2
Temperature profile comparison of Argo and COAWST coupling models near the typhoon path before and after the passage of No. 1709 typhoon “Nesat”. The dashed blue line in the figure (a) is the 169th profile data of No. 2902656 Argo, the solid red line is the temperature profile of COAWST simulation results, and the dashed blue line in the figure (b) is the 170th profile data of No. 2902656 Argo, the solid red line is the temperature profile of COAWST simulation results"
Fig. 6
Temporal and spatial characteristics of the variation amplitude of SST, MLT and TT induced by typhoon samples. (a) The average SST before the typhoon; (b) the average reduction of SST during typhoon transit; (c) the average reduction of SST within 7 days after the passage of the typhoon; (d) average MLT before the typhoon; (e) the average increase of MLT during typhoon transit; (f) the average increase in MLT within 7 days after the typhoon’s passage; (g) average TT before the typhoon; (h) the average reduction of TT during typhoon transit; (i) average reduction of TT within 7 days after the typhoon’s passage. The black box area is the main impact area of the turning typhoon. The area in blue box is the main affected area of the northwestward typhoon. The area in the red box is the main impact area of the westward typhoon. The blank area in the figure is the area not affected by the typhoon samples"
Fig. 7
The average SST (a), MLT (b) and TT (c) from July to September in the mean affect area from 2001 to 2020 (https://data.marine.copernicus.eu/product/GLOBAL_REANALYSIS_PHY_001_031/), the red, blue and black boxes in the figure show the main affect area of the westward typhoon, the northwestward typhoon and the turning typhoon respectively"
Tab. 8
Background field information of the main affect areas of each type of typhoon"
主要影响区域内SST平均值/℃ | 主要影响区域内MLT平均值/m | 主要影响区域内TT平均值/m | ||||
---|---|---|---|---|---|---|
过境前2d平均 | 7—9月平均 | 过境前2d平均 | 7—9月平均 | 过境前2d平均 | 7—9月平均 | |
西行路径台风 | 28.49 | 29.28 | 24.08 | 29.01 | 106.05 | 118.02 |
西北路径台风 | 29.21 | 29.56 | 25.74 | 27.51 | 100.27 | 114.98 |
转向路径台风 | 27.25 | 27.54 | 13.46 | 14.59 | 21.14 | 38.95 |
Fig. 8
The number of mesoscale cold vortices from July to September in the mean affect area from 2002 to 2021, using AVISO altimetry data (https://data.aviso.altimetry.fr/aviso-gateway/data/META3.1exp_DT/META3.1exp_DT_twosat/), the red, blue and black boxes in the figure show the main affect area of the westward typhoon, the northwestward typhoon and the turning typhoon respectively"
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