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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Total article views: 2,413 (including HTML, PDF, and XML)
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1,866
488
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BibTeX: 69
EndNote: 93
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399
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8
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HTML: 399
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Total: 633
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Cumulative views and downloads
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Viewed (geographical distribution)
Total article views: 3,046 (including HTML, PDF, and XML)
Thereof 3,046 with geography defined
and 0 with unknown origin.
Total article views: 2,413 (including HTML, PDF, and XML)
Thereof 2,413 with geography defined
and 0 with unknown origin.
Total article views: 633 (including HTML, PDF, and XML)
Thereof 620 with geography defined
and 13 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...
