Diurnal cycle and seasonal variation of cloud cover over the Tibetan Plateau as determined from Himawari-8 new-generation geostationary satellite data

Abstract Analysis of cloud cover and its diurnal variation over the Tibetan Plateau (TP) is highly reliant on satellite data; however, the accuracy of cloud detection from both polar-orbiting and geostationary satellites over this area remains unclear. The new-generation geostationary Himawari-8 sat...

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Main Authors: Huazhe Shang, Husi Letu, Takashi Y. Nakajima, Ziming Wang, Run Ma, Tianxing Wang, Yonghui Lei, Dabin Ji, Shenshen Li, Jiancheng Shi
Format: Article
Language:English
Published: Nature Portfolio 2018-01-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-018-19431-w
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author Huazhe Shang
Husi Letu
Takashi Y. Nakajima
Ziming Wang
Run Ma
Tianxing Wang
Yonghui Lei
Dabin Ji
Shenshen Li
Jiancheng Shi
author_facet Huazhe Shang
Husi Letu
Takashi Y. Nakajima
Ziming Wang
Run Ma
Tianxing Wang
Yonghui Lei
Dabin Ji
Shenshen Li
Jiancheng Shi
author_sort Huazhe Shang
collection DOAJ
description Abstract Analysis of cloud cover and its diurnal variation over the Tibetan Plateau (TP) is highly reliant on satellite data; however, the accuracy of cloud detection from both polar-orbiting and geostationary satellites over this area remains unclear. The new-generation geostationary Himawari-8 satellites provide high-resolution spatial and temporal information about clouds over the Tibetan Plateau. In this study, the cloud detection of MODIS and AHI is investigated and validated against CALIPSO measurements. For AHI and MODIS, the false alarm rate of AHI and MODIS in cloud identification over the TP was 7.51% and 1.94%, respectively, and the cloud hit rate was 73.55% and 80.15%, respectively. Using hourly cloud-cover data from the Himawari-8 satellites, we found that at the monthly scale, the diurnal cycle in cloud cover over the TP tends to increase throughout the day, with the minimum and maximum cloud fractions occurring at 10:00 a.m. and 18:00 p.m. local time. Due to the limited time resolution of polar-orbiting satellites, the underestimation of MODIS daytime average cloud cover is approximately 4.00% at the annual scale, with larger biases during the spring (5.40%) and winter (5.90%).
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spelling doaj.art-e0c3e2c9c3274f4d961205a8eb77ddfe2022-12-21T23:37:36ZengNature PortfolioScientific Reports2045-23222018-01-01811810.1038/s41598-018-19431-wDiurnal cycle and seasonal variation of cloud cover over the Tibetan Plateau as determined from Himawari-8 new-generation geostationary satellite dataHuazhe Shang0Husi Letu1Takashi Y. Nakajima2Ziming Wang3Run Ma4Tianxing Wang5Yonghui Lei6Dabin Ji7Shenshen Li8Jiancheng Shi9State Key Laboratory of Remote Sensing Science, Institute of Remote Sensing and Digital Earth, Chinese Academy of SciencesState Key Laboratory of Remote Sensing Science, Institute of Remote Sensing and Digital Earth, Chinese Academy of SciencesResearch and Information Center, Tokai UniversityState Key Laboratory of Remote Sensing Science, Institute of Remote Sensing and Digital Earth, Chinese Academy of SciencesState Key Laboratory of Remote Sensing Science, Institute of Remote Sensing and Digital Earth, Chinese Academy of SciencesState Key Laboratory of Remote Sensing Science, Institute of Remote Sensing and Digital Earth, Chinese Academy of SciencesState Key Laboratory of Remote Sensing Science, Institute of Remote Sensing and Digital Earth, Chinese Academy of SciencesState Key Laboratory of Remote Sensing Science, Institute of Remote Sensing and Digital Earth, Chinese Academy of SciencesState Key Laboratory of Remote Sensing Science, Institute of Remote Sensing and Digital Earth, Chinese Academy of SciencesState Key Laboratory of Remote Sensing Science, Institute of Remote Sensing and Digital Earth, Chinese Academy of SciencesAbstract Analysis of cloud cover and its diurnal variation over the Tibetan Plateau (TP) is highly reliant on satellite data; however, the accuracy of cloud detection from both polar-orbiting and geostationary satellites over this area remains unclear. The new-generation geostationary Himawari-8 satellites provide high-resolution spatial and temporal information about clouds over the Tibetan Plateau. In this study, the cloud detection of MODIS and AHI is investigated and validated against CALIPSO measurements. For AHI and MODIS, the false alarm rate of AHI and MODIS in cloud identification over the TP was 7.51% and 1.94%, respectively, and the cloud hit rate was 73.55% and 80.15%, respectively. Using hourly cloud-cover data from the Himawari-8 satellites, we found that at the monthly scale, the diurnal cycle in cloud cover over the TP tends to increase throughout the day, with the minimum and maximum cloud fractions occurring at 10:00 a.m. and 18:00 p.m. local time. Due to the limited time resolution of polar-orbiting satellites, the underestimation of MODIS daytime average cloud cover is approximately 4.00% at the annual scale, with larger biases during the spring (5.40%) and winter (5.90%).https://doi.org/10.1038/s41598-018-19431-w
spellingShingle Huazhe Shang
Husi Letu
Takashi Y. Nakajima
Ziming Wang
Run Ma
Tianxing Wang
Yonghui Lei
Dabin Ji
Shenshen Li
Jiancheng Shi
Diurnal cycle and seasonal variation of cloud cover over the Tibetan Plateau as determined from Himawari-8 new-generation geostationary satellite data
Scientific Reports
title Diurnal cycle and seasonal variation of cloud cover over the Tibetan Plateau as determined from Himawari-8 new-generation geostationary satellite data
title_full Diurnal cycle and seasonal variation of cloud cover over the Tibetan Plateau as determined from Himawari-8 new-generation geostationary satellite data
title_fullStr Diurnal cycle and seasonal variation of cloud cover over the Tibetan Plateau as determined from Himawari-8 new-generation geostationary satellite data
title_full_unstemmed Diurnal cycle and seasonal variation of cloud cover over the Tibetan Plateau as determined from Himawari-8 new-generation geostationary satellite data
title_short Diurnal cycle and seasonal variation of cloud cover over the Tibetan Plateau as determined from Himawari-8 new-generation geostationary satellite data
title_sort diurnal cycle and seasonal variation of cloud cover over the tibetan plateau as determined from himawari 8 new generation geostationary satellite data
url https://doi.org/10.1038/s41598-018-19431-w
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