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Analysis of upper ocean response to Typhoon Doksuri in the northwest South China Sea
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Qian Zhang1, Guanghong Liao1, 2, *, Feilong Lin1, Weifang Jin1, Chujin Liang1
Haiyang Xuebao | 2019, 41(7) : 22 - 35
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Haiyang Xuebao | 2019, 41(7): 22-35
Physical Oceanography, Marine Meteorology and Marine Physics
Analysis of upper ocean response to Typhoon Doksuri in the northwest South China Sea
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Qian Zhang1, Guanghong Liao1, 2, *, Feilong Lin1, Weifang Jin1, Chujin Liang1
Affiliations
  • 1 State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Minisitry of Natural Resources, Hangzhou 310012, China
  • 2 College of Oceanography, Hohai University, Nanjing 210098, China
Published: 2019-07-25 doi: 10.3969/j.issn.0253-4193.2019.07.003
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Based on the in-situ data from mooring deployed in the northwest South China Sea, we investigate the dynamical and thermal dynamical response of upper ocean to Typhoon Doksuri. In the aspect of dynamic response, as the Typhoon passing, the currents in upper layer enhanced strikingly, the zonal currents in the mixed layer reaches 1.20 m/s. After the passage of Typhoon Doksuri, the currents in the upper layer are dominated by near-inertial oscillation, which rotate clockwise with a period between 36–40 hours. The kinetic energy of near-inertial wave shows two high energetic cores in vertical, which locates at the mixed layer and the thermocline layer, respectively. The estimated e-folding time-scale of near-inertial energy decay is about 3.7 d, and we believe that the downward propagation of energy is the major reason for the decay. The power spectra analysis of currents reveals that power density at inertial frequency, during the period of Typhoon Doksuri, increases about 29.4 times larger than that before the Typhoon arriving. Nevertheless, power density both at diurnal (K1) and semidiurnal (M2) frequency decreases during Typhoon period. Additionally, a blue shift at inertial frequency is identified. We find that the averaged near-internal frequency in upper 400 m is 1.167 f0 for zonal near-inertial currents and 1.170 f0 for meridional near-inertial currents (where f0 is the local inertial frequency). This blue shift is connected with the downward propagation of near-inertial waves and input of positive relative vorticity. In the aspect of thermodynamic response, the temperature rises in the upper layer between 40–250 m depth, due to the stirring induced by strong wind, and the maximum increased temperature amplitude is about 1℃. In addition, the decrease of salinity above 70 m may be related to the precipitation caused by the Typhoon. While the upwelling induced by Ekman pumping may have significant contribution to the increase of salinity at the depth of 70–100 m.

near-inertial oscillations  /  energy spectrum  /  dynamic response  /  thermodynamic response  /  South China Sea
Qian Zhang, Guanghong Liao, Feilong Lin, Weifang Jin, Chujin Liang. Analysis of upper ocean response to Typhoon Doksuri in the northwest South China Sea[J]. Haiyang Xuebao, 2019 , 41 (7) : 22 -35 . DOI: 10.3969/j.issn.0253-4193.2019.07.003
Year 2019 volume 41 Issue 7
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Article Info
doi: 10.3969/j.issn.0253-4193.2019.07.003
  • Receive Date:2018-07-04
  • Online Date:2026-04-02
  • Published:2019-07-25
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  • Received:2018-07-04
  • Revised:2018-10-09
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    1 State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Minisitry of Natural Resources, Hangzhou 310012, China
    2 College of Oceanography, Hohai University, Nanjing 210098, China
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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