1) diurnal variation of the tropical convection
热带对流日变化
2) tropical convection
热带对流
1.
The seasonal and interannual variability of intraseasonal oscillation(ISO) intensity of tropical convection is investigated by using NCAR/NOAA outgoing longwave radiation(OLR) data,along with the relationship with sea surface temperature(SST).
利用外逸长波辐射(outgoing longwave radiation,OLR)资料分析了热带对流季内振荡(ISO)强度的季节变化及年际异常特征,重点研究其与海表温度的关系。
3) tropical convective cloud
热带对流云
4) tropical deep convection
热带深对流
1.
The WRF model configurative with high resolution and NCEP 1°×1° reanalysis data were used to simulate the development of a tropical deep convection on the Tiwi Islands, north Australia, and to investigate the sensitivity of model results to model resolutions and microphysical parameterization schemes.
利用WRF(Weather Research Forecast)模式和1°×1°NCEP全球分析资料对2005年11月16日澳大利亚北部Tiwi岛上的一次热带深对流个例进行了数值模拟,对模式网格分辨率和微物理参数化方案的影响进行了敏感性试验,并与实测资料进行了对比。
5) stemflow daily change
茎流日变化
补充资料：热带
1.赤道两侧南回归线和北回归线之间的地带称"热带"，也叫"回归带"。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条