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三亚降水日变化特征及其影响机制

蓝欣 冯箫

海洋预报2024,Vol.41Issue(6):71-81,11.
海洋预报2024,Vol.41Issue(6):71-81,11.DOI:10.11737/j.issn.1003-0239.2024.06.008

三亚降水日变化特征及其影响机制

Characteristics and mechanisms of diurnal variation of precipitation in Sanya

蓝欣 1冯箫2

作者信息

  • 1. 海南省南海气象防灾减灾重点实验室,海南海口 570203||海南省三亚市气象局,海南三亚 572000
  • 2. 海南省南海气象防灾减灾重点实验室,海南海口 570203||海南省气象台,海南海口 570203
  • 折叠

摘要

Abstract

Based on hourly precipitation data during 2011-2020,the characteristics and mechanisms of diurnal variation of precipitation in Sanya from June to October are studied.The results show that diurnal variation of precipitation in Sanya exhibits a bimodal pattern,with a primary peak at 05-08 LST and a secondary peak at 15-17 LST.Spatial distribution differences are observed in the diurnal variation,with peak values predominantly in the afternoon for inland mountainous areas and in the morning for coastal areas.Rainy days are divided into days with early morning peaks and days with afternoon peaks.In terms of atmospheric circulation,early morning peak rainfall days are featured by consistent westward low-eastward high pattern in the geopotential height anomaly along with southeaster anomaly,while afternoon peak rainfall days are featured by a low-pressure anomaly near 115°E over the South China Sea and northeaster anomaly.Regarding the influencing mechanisms,for morning peak rainfall days,there is a low-pressure anomaly and positive specific humidity anomaly at night.Continuous strong convergence is present near the surface in the Sanya region,accompanied by a deep ascending motion system in the vertical circulation,which is the primary factor leading to nighttime precipitation.For afternoon peak rainfall days,negative specific humidity anomalies are observed at night,and a deep descending circulation prevails at 500~600 hPa in the vertical circulation,suppressing nighttime precipitation.Local wind circulation in the afternoon leads to persistent strong near-surface convergence anomalies near the mountainous areas.Throughout the vertical circulation,there is a deep ascending motion circulation,serving as the main reason for afternoon precipitation.

关键词

降水日变化/三亚/晨峰雨日/午峰雨日

Key words

diurnal variation of precipitation/Sanya/early morning peak rainy days/afternoon peak rainy days

分类

天文与地球科学

引用本文复制引用

蓝欣,冯箫..三亚降水日变化特征及其影响机制[J].海洋预报,2024,41(6):71-81,11.

基金项目

海南省气象局青年基金项目(hnqxSJ202126). (hnqxSJ202126)

海洋预报

OA北大核心CSTPCD

1003-0239

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