Material to : Seasonal Versus Permanent Thermocline Warming by Tropical Cyclones
Material to : Seasonal Versus Permanent Thermocline Warming by Tropical Cyclones
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DOI:
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发表时间:
2010
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影响因子:
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通讯作者:
M. Jansen;R. Ferrari;T. Mooring
中科院分区:
文献类型:
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作者:
M. Jansen;R. Ferrari;T. Mooring
The heat uptake in TC cold wakes is computed along cross-sections centered on each of the 6-hourly Best Track locations. For storms moving predominantly meridionally (i.e. within 45) we compute zonal cross-sections and for storms moving predominantly zonally, we compute meridional cross-sections. The heat uptake per unit area along each 6-hourly cross-section is then multiplied by the distance to the next 6-hourly location. To calculate the total heat transport we now need to integrate across the wake, which poses a question as to what is an appropriate choice for the width of the cross sections. In the absence of any background variability of SST, the heat uptake estimate would not depend on this choice, as long as the width is sufficiently large to include the whole TC signal. However, background variability in SST will bias the heat uptake estimate high, especially far from the wake center. The reason is that equations (1) and (2) return a positive heat uptake estimate whenever there is a decrease in SST, but zero heat uptake when there is an increase in SST. This is appropriate if the SST anomalies are associated with the passage of the storm but not if the SST variations are due to background variability. Background SST variations are not expected to correspond to a net heat uptake, but our algorithm always returns positive values associated with warming of cold anomalies and zero values