感热通量

感热通量平均值及其年际变化的距平值均比潜热通量的要小一个量级。

Average sensible heat flux and its interannual variations of anomalies are smaller an order of magnitude than that of the latent heat flux .

除了东海，潜热通量的年均值基本上表现为自北向南减小的分布，而感热通量年均值则表现为自北向南增大的分布。

In addition , except for the East China sea , the latent heat flux generally indicates a decreased distribution from north to south , while the annual averaged sensible heat flux shows an increased distribution .

风向对LAS和EC观测感热通量值有显著影响。

Wind direction has a significant effect on sensible heat flux by LAS and EC .

潜热和感热通量能使SST的下降的最大值为3℃。

And latent heat and sensible heat fluxes could make the SST decrease 3 ℃ .

在此基础上，利用LAS的观测结果对丘陵地区地表感热通量的变化特征进行了分析研究，首次揭示了四川盆地丘陵地区地气相互作用的一些新事实。

Furthermore , the characteristics of ground surface sensible flux change is analyzed according to the LAS data .

下垫面不均匀性对LAS和EC的感热通量差异影响显著。

Which indicates that : the inhomogeneity of underlying surface has a significant influence on difference of sensible heat flux by LAS and EC .

雨天状况下，各种植被间标量粗糙度的差异减小了。计算的地表温度、感热通量、潜热通量较原BATS的更为合理。

The calculated land surface temperature , sensible heat flux andlatent heat flux is more reasonable than those in unchanged BATS .

拟合得到最适稳定度普适函数fTGuyuan，并通过比较不同方法得到的感热通量，证实fTGuyuan函数是合理可靠的。

The function fT_Guyuan was proved to be reasonable and reliable by comparing different calculation methods for sensible heat flux .

对于东海而言，风速、降雨、海-气温差和SST变化与感热通量都有较好的相关性。

As for East China Sea , wind speed , precipitation , difference in air-sea temperature and SST change depicts fairly good agreement with the sensible heat flux .

NEP区和NWP区夏季的海气温差、感热通量、潜热通量有明显的差异。

There are distinct differences of air-sea temperature difference , latent heat and sensible heat flux between NEP and NWP .

春季南海海面潜热通量和感热通量与短波辐射和风应力相比较，是一个对SST影响较小的量。

Compared with solar short wave radiation and wind stress , the latent heat and sensible heat flux are a minor factor in controlling the variable of the SST in spring .

密云站LAS观测得到的感热通量与涡动相关的相比，日变化特征更加平滑，且空间代表性更大。

It was also found that the sensible heat flux diurnal variation obtained by LAS in Miyun Station was smoother and with greater spatial representation when it compared to EC measurements .

但8月份的潜热通量大，平均最大约为120W·m-2，当有降水发生时，潜热通量可达570W·m-2，与感热通量相当。

But latent heat flux can be up to 570 W · m - 2 , when precipitation occuring .

EC观测的感热通量和潜热通量都与模式模拟结果存在很大的差异，LAS缩小了这种误差，改进了地表能量平衡。

There is a great difference between both sensible heat flux and latent heat flux observed by EC and which simulated by model , while the observation of LAS reduced the fault bit , which improved the Surface energy balance .

净辐谢Rn是感热通量的主要驱动因子，HLAs-HEC在生长季的值大于非生长季的值，并与Rn成正相关。

Net radiation Rn is the main driving factor to sensible heat flux . The value of HLAS-HEC in the growing season is greater than the value in the non-growing season and positively correlated with Rn .

利用COADS资料，首先计算了1949－1979年逐月北太平洋洋面的潜热通量与感热通量之和，并进行EOF分解，然后分析它们的时空变化特征。

The COADS data are used to estimate the sum of monthly latent and sensible heat fluxes ( simplified as head flux hereafter ) over the sea surface in the North Pacific from 1949 to 1979 . Then their time and space variations are analyzed using the EOF method .

而中尺度感热通量的强弱受多种因素的制约。

The mesoscale sensible heat flux is influenced by many facts .

区域平均感热通量与蒸散量相比在此期间变化并不明显。

The sensible heat fluxes show no obvious variation in this period .

用涡度相关方法，观测了感热通量和潜热通量，对模型进行了验证。

The model was validated with the data measured by eddy covariance method .

热带大西洋海表潜热和感热通量的季节和年际变化研究

Seasonal-to-Interannual Variability of Latent and Sensible Heat Fluxes in the Tropical Atlantic Ocean

绿洲农田作物的显热和潜热输送关于棉田感热通量和潜热通量的几种计算方法

Sensible heat and latent heat transportation in Oasis cropland

亚洲季风区地面感热通量的区域变化特征

Characteristics of spatial variation of surface sensible heat flux in Asian monsoon region

风浪条件与感热通量具有较好的相关性，相关系数达0.67。

The correlation coefficient between wind wave condition and sensible heat flux is 0.67 .

发生较强降水时，感热通量和潜热通量均较小，在强降水之后如遇晴朗天气，则潜热通量较大。

When heavy rain occurred , both of sensible and latent heat fluxes were smaller .

绿洲地区感热通量小，潜热通量大；

Big and Good Matter Oasis has low sensible heat flux and high latent heat flux ;

7月份感热通量比6月份大约减少了2/3以上。

The sensible heat flux is less about 2 / 3 in July than that in June .

感热通量和潜热通量的季节动态与净辐射基本一致，均受降水影响。

The patterns of sensible and latent heat fluxes and net solar radiation were affected by precipitation .

分析结果表明在赤道海域，潜热通量远远大于感热通量。

The results show that the latent heat flux is much greater than the ra-diate heat flux .

地表感热通量明显大于地表潜热通量；

The sensible heat flux is very greater than the latent heat flux in the PBL air .

积云对流凝结加热和洋面上的潜热感热通量；

The cumulus convective condensation heating and the latent and sensible heat fluxes on the sea surface ;