1) deep convection
深对流
1.
Based on FY-2C hourly infrared T_(BB) dataset from June to August in 2007,the distribution and spatiotemporal variations of deep convection over China and its vicinity during the summer of 2007 is analyzed and compared with the atmospheric circulation background based on the NCEP final analysis dataset and the climatological distribution of deep convection based on 10-year T_(BB) dataset.
利用逐时FY-2C卫星红外亮温(T_(BB))资料讨论了2007年夏季(6—8月)我国深对流活动的时空演变特征,并同10年的深对流活动特征进行了对比分析。
3) deep convective system
深对流系统
1.
Although potential vorticity is a common and useful physical quantity for meteorological analysis,it is a little weak in deep convective systems due to the apparent slant of moist isentropic surfaces.
位涡在诊断分析中是一个常用且有效的物理量,但在深对流系统中由于湿等熵面的倾斜变得较弱。
4) Deep convection heating
深对流加热
1.
Based on 1948-1999 NCEP/NCAR data of the deep convection heating and monthly-mean rainfall at 160 stations, study is undertaken of summertime deep convection heating over the southeast of Tibetan Plateau.
文章利用 1948～ 1999年NCEP/NCAR全球深对流加热率再分析资料和 195 1～ 2 0 0 1年全国 16 0站月平均降水量研究了中国区域夏季深对流加热分布状况 ,青藏高原东南部夏季深对流加热较强 ,是潜热释放较多和深对流活动旺盛区域 ;青藏高原东南部深对流加热率与长江中下游地区降水的相关分析也表明 ,夏季青藏高原东南部深对流活动对长江中下游地区夏季降水偏多有重要影响 ,可以为长江中下游地区夏季降水提供水分和能量。
5) oceanic deep convection
海洋深对流
6) 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。
补充资料：热深厥深
热深厥深 热深厥深 病证名。指热厥证的征象。指邪热越深入，四肢厥冷的症状越严重，皆因阳气被遏，邪气内闭所致。属真热假寒证。
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