典型厄尔尼诺期间台风降水δ18O变化分析: 以2018年22号台风“山竹”为例

doi:10.11978/2019081

Abstract

Abstract:

The rainfall caused by typhoon is different from the other precipitation event due to its unique physical structure. The stable isotope composition of typhoon precipitation is also quite different from that of a general precipitation event. Based on meteorological data before and after the landing of Typhoon Mangkhut (2018) in Guangzhou and Dongguan and stable isotope data of precipitation at hourly resolution, we analyzed the characteristics of the stable isotope variation of the typhoon precipitation and its influencing factors. During the influence of Typhoon Mangkhut, the δ¹⁸O value of precipitation in Guangzhou ranged from -5.7‰~-19.2‰, with a variation of 13.5‰; and the average value was -15.5‰. The variation of δ¹⁸O value in Dongguan was -7.3‰~-20.0‰, with a variation of 12.7‰; and the average was -14.8‰. The variations of δ¹⁸O value of precipitation in the two places both showed the three-stage variation characteristics of inverted U-shape. Due to the influence of evaporation, the precipitation oxygen isotope values in the typhoon at the front and back were relatively positive in two places, of which Guangzhou was (-5.7‰~-9.3‰, and Dongguan was -7.3‰~-8.1‰. The stable isotope values of precipitation in the typhoon central area of the two places were extremely negative, ranging from -16.0‰ to -19.2‰ (Guangzhou) and from -13.0‰ to -20.0‰ (Dongguan), which were the most negative precipitation δ¹⁸O values reported in this region so far. According to the analysis, the generated distant typhoon intensity was enhanced during the El Ni?o. Thus, the stronger convection and water-vapor circulation in Typhoon Mangkhut (2018) led to extreme negative δ ¹⁸O value of its precipitation.

Key words: Typhoon Mangkhut (2018), δ¹⁸O value of precipitation, microphysical process, El Ni?o

CLC Number:

P732.3

Yunyue YANG, Tao XU, Cuiyu LUO, Juan LIU, Xiuyang JIANG. Analysis on the variation of typhoon precipitation δ ¹⁸O during typical El Niño event: A case study of Typhoon Mangkhut (2018)[J].Journal of Tropical Oceanography, 2020, 39(4): 34-41.

Figures/Tables 5

Fig. 1

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Tab. 1

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年份	台风名称	最负δ¹⁸O值/‰	采样地点
2018	山竹	-19.2	广州
2018	山竹	-20.0	东莞
2004	圆规	-8.2	广州
2004	南川	-13.1	广州
2007	帕布	-14.1	广州
2007—2009	--	-17.7~-16.4	广州
2013—2017	--	-11.4~-17.9	福州

Analysis on the variation of typhoon precipitation δ ¹⁸O during typical El Niño event: A case study of Typhoon Mangkhut (2018)

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Analysis on the variation of typhoon precipitation δ 18O during typical El Niño event: A case study of Typhoon Mangkhut (2018)

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Analysis on the variation of typhoon precipitation δ ¹⁸O during typical El Niño event: A case study of Typhoon Mangkhut (2018)