Surface diurnal warming in the East China Sea derived from satellite remote sensing

宋丹; 段志刚; 翟方国; 何齐齐

doi:10.1007/s00343-018-7035-7

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Surface diurnal warming in the East China Sea derived from satellite remote sensing

Physics | Updated：2023-05-19

- Surface diurnal warming in the East China Sea derived from satellite remote sensing
- Surface diurnal warming in the East China Sea derived from satellite remote sensing
- 海洋湖沼学报（英文） 2018年36卷第3期页码：620-629
- Affiliations：
  
  1.Institute of Physical Oceanography, Ocean College, Zhejiang University, Zhoushan 316021, China
  2.State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310021, China
  3.College of Oceanic and Atmospheric Sciences, Ocean University of China, Qingdao 266100, China
- Author bio：
  
  ZHAI Fangguo, gfzhai@ouc.edu.cn
- Funds：
  
  the Zhejiang Provincial Natural Science Foundation(LY17D060003);the Shandong Provincial Natural Science Foundation(ZR2015DQ006);the National Narutal Science Foundation of China(41306035);the National Narutal Science Foundation of China(41206006);the National Key Research and Development Program of China(2016YFC1401404)
- DOI：10.1007/s00343-018-7035-7
  中图分类号：
- 收稿：2017-02-23，
  
  录用：2017-3-9，
  
  网络首发：2017-04-17，
  
  纸质出版：2018-05
- Accepted：
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宋丹, 段志刚, 翟方国, 等. Surface diurnal warming in the East China Sea derived from satellite remote sensing[J]. 海洋湖沼学报（英文）, 2018,36(3):620-629.

Dan SONG, Zhigang DUAN, Fangguo ZHAI, et al. Surface diurnal warming in the East China Sea derived from satellite remote sensing[J]. Chinese Journal of Oceanology and Limnology, 2018, 36(3): 620-629.
宋丹, 段志刚, 翟方国, 等. Surface diurnal warming in the East China Sea derived from satellite remote sensing[J]. 海洋湖沼学报（英文）, 2018,36(3):620-629. DOI： 10.1007/s00343-018-7035-7.

Dan SONG, Zhigang DUAN, Fangguo ZHAI, et al. Surface diurnal warming in the East China Sea derived from satellite remote sensing[J]. Chinese Journal of Oceanology and Limnology, 2018, 36(3): 620-629. DOI： 10.1007/s00343-018-7035-7.

摘要

Abstract

Process of sea surface diurnal warming has drawn a lot of attention in recent years

but that occurs in shelf seas was rarely addressed. In the present work

surface diurnal warming strength in the East China Sea was calculated by the sea surface temperature (SST) data derived from the MODIS sensors carried by the satellites Aqua and Terra. Due to transit time difference

both the number of valid data and the surface diurnal warming strength computed by the MODIS-Aqua data are relatively larger than Terra. Therefore

the 10-year MODIS-Aqua data from 2005 to 2014 were used to analyze the monthly variability of the surface diurnal warming. Generally

the surface diurnal warming in the East China sea is stronger in summer and autumn but weaker in winter and spring

while it shows different peaks in different regions. Large events with Δ

≥ 5 K have also been discussed. They were found mainly in coastal area

especially near the Changjiang (Yangtze) River estuary. And there exists a high-incidence period from April to July. Furthermore

the relationship between surface diurnal warming and wind speed was discussed. Larger diurnal warming mainly lies in areas with low wind speed. And its possibility decreases with the increase of wind speed. Events with Δ

≥ 2.5 K rarely occur when wind speed is over 12 m/s. Study on surface diurnal warming in the East China Sea may help to understand the daily scale air-sea interaction in the shelf seas. A potential application might be in the marine weather forecasts by numerical models. Its impact on the coastal eco-system and the activities of marine organisms can also be pursued.

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references

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