College of Global Change and Earth System Science, and State Key
Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal
University, Beijing 100875, China
College of Global Change and Earth System Science, and State Key
Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal
University, Beijing 100875, China
Xingchuan Yang
College of Global Change and Earth System Science, and State Key
Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal
University, Beijing 100875, China
College of Global Change and Earth System Science, and State Key
Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal
University, Beijing 100875, China
Ping Zhou
College of Global Change and Earth System Science, and State Key
Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal
University, Beijing 100875, China
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1,808
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Total: 2,352
BibTeX: 36
EndNote: 42
Views and downloads (calculated since 04 Oct 2021)
Cumulative views and downloads
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Total article views: 1,781 (including HTML, PDF, and XML)
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1,435
309
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1,781
30
33
HTML: 1,435
PDF: 309
XML: 37
Total: 1,781
BibTeX: 30
EndNote: 33
Views and downloads (calculated since 12 Jan 2022)
Cumulative views and downloads
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Total article views: 571 (including HTML, PDF, and XML)
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373
182
16
571
6
9
HTML: 373
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Total: 571
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EndNote: 9
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Cumulative views and downloads
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Viewed (geographical distribution)
Total article views: 2,352 (including HTML, PDF, and XML)
Thereof 2,418 with geography defined
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Total article views: 1,781 (including HTML, PDF, and XML)
Thereof 1,861 with geography defined
and -80 with unknown origin.
Total article views: 571 (including HTML, PDF, and XML)
Thereof 557 with geography defined
and 14 with unknown origin.
Using multi-year data, this study reveals the slump of sea land breeze (SLB) at Brisbane during mega fires and investigates the impact of fire-induced aerosols on SLB. Different aerosols have different impacts on sea wind (SW) and land wind (LW). Aerosols cause the decrease of SW, partially offset by the warming effect of black carbon (BC). The large-scale cooling effect of aerosols on sea surface temperature (SST) and the burst of BC contribute to the slump of LW.
Using multi-year data, this study reveals the slump of sea land breeze (SLB) at Brisbane during...