The studies of heat flux space - time variability are limited because of the poor qualities of heat fluxes datasets 但受热通量资料质量的局限，目前关于热通量的时空变化的研究不多。
There are negative latent and sensible heat fluxes in south and east of the cyclone central area after it moved to ocean 气旋出海后在气旋中心区南方和东方存在负潜热通量和感热通量区。
Standard test method for steady - state heat flux measurements and thermal transmission properties by means of the guarded - hot - plate apparatus 用护热板法测定稳态热通量和传导性的标准试验方法
The distribution and variation of latent and sensible heat fluxes of the cyclones were discussed based on the numerical simulation 在数值模拟基础上重点讨论了出海气旋发展过程潜热通量和感热通量的分布及其演变情况。
A strong positive heat flux area in the front of cyclone may be one of important reasons for eastward movement and development of cyclone going to sea 出海气旋的东移和发展，其前方强大正热通量区的存在可能是重要原因之一。
South china sea gain heat by yearly average with 58wm - 2 . a maximum of heat loss exists in kuroshio area and it can get - 330 wm - 2 in december 在黑潮流区存在最大的净热通量损失值区，在冬季12月份最大损失值可达- 300wm ~ ( - 2 ) 。
And this research also proves that heat flux influence predominantly the sst , but the impact of wind stress can reach the levels behind the isothermal layer 研究还证明了热通量对海温的影响主要出现在表层，而风应力的影响可以达到等温层以下。
The mld of the ocean near the equator from 10 ? s to 10 ? n are less than 50 m and have no evident seasonal variability 而在10 s 10 n之间的赤道附近海域，因风应力和净热通量的季节变化不大，且该区降水量较大，浮力通量增加， mld较浅，低于50米，且没有明显的季节变化。
The variation of sensible heat flux is dominated by air - sea temperature difference . interannual variability of turbulent heat fluxes is examined using svd , eof and mtm methods 热带太平洋enso事件通过对walker环流的调整减小热带大西洋itcz区的风速值，湍动热通量亦随之减小。
It has discovered common faults of various experimental collections and agreed well with the chf data of annular tubes and rectangular channels in water and other liquids 理论式和本实验及其他文献的套管，长方形通道的最大热通量实验数据进行了比较，在流路狭长的情况时两者相当吻合。
