The Footprint of Atlantic Multidecadal Oscillation on the Intensity of Tropical Cyclones Over the Western North Pacific

The Footprint of Atlantic Multidecadal Oscillation on the Intensity of Tropical Cyclones Over the Western North Pacific
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大西洋数十年振荡对西北太平洋热带气旋强度的影响

DOI:
10.3389/feart.2020.604807
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发表时间:
2020-11
影响因子:
2.9
通讯作者:
Li Xiang
Li Xiang
中科院分区:
地球科学3区
文献类型:
--
作者:
Sun Cheng;Liu Yusen;Gong Zhanqiu;Kucharski Fred;Li Jianping;Wang Qiuyun;Li Xiang

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北太平洋西部(WNP)上的海面温度(SST)表现出对多年龄变化的强大衰落,在该地区,温水为热带气旋(TCS)燃烧。观察记录显示WNP TC Met中有明显的decadal变化
Sea surface temperature (SST) over the western North Pacific (WNP) exhibits strong decadal to multidecadal variability and in this region, warm waters fuel the tropical cyclones (TCs). Observational records show pronounced decadal variations in WNP TC metrics during 1950–2018. Statistical analysis of the various TC metrics suggests that the annual average intensity of WNP TCs is closely linked to the AMO (r = 0.86 at decadal timescales, p < 0.05). Observations and coupled atmosphere-ocean simulations show that the decadal WNP SST variations regarded as the primary driver of TC intensity, are remotely controlled by the AMO. Corresponding to the WNP SST warming, the local SLP gets lower and the tropospheric air becomes warmer and moister, enhancing atmospheric instability and the generation of convective available potential energy. These favorable changes in the background environment provide more “fuel” to the development of deep convection and intensify the WNP TCs. The footprints of AMO in WNP SST and atmospheric states through trans-basin interaction eventually exert a significant impact on the TC intensity over the WNP region.
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