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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1,704
470
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2,218
29
33
HTML: 1,704
PDF: 470
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Total: 2,218
BibTeX: 29
EndNote: 33
Views and downloads (calculated since 04 Oct 2021)
Cumulative views and downloads
(calculated since 04 Oct 2021)
Total article views: 1,654 (including HTML, PDF, and XML)
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1,332
292
30
1,654
23
24
HTML: 1,332
PDF: 292
XML: 30
Total: 1,654
BibTeX: 23
EndNote: 24
Views and downloads (calculated since 12 Jan 2022)
Cumulative views and downloads
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Total article views: 564 (including HTML, PDF, and XML)
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372
178
14
564
6
9
HTML: 372
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Total: 564
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EndNote: 9
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Cumulative views and downloads
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Viewed (geographical distribution)
Total article views: 2,218 (including HTML, PDF, and XML)
Thereof 2,284 with geography defined
and -66 with unknown origin.
Total article views: 1,654 (including HTML, PDF, and XML)
Thereof 1,734 with geography defined
and -80 with unknown origin.
Total article views: 564 (including HTML, PDF, and XML)
Thereof 550 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...
