潜热通量

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 .

潜热通量、显热通量、净辐射、光合有效辐射均与CO2通量呈极显著正相关。

Latent heat flux , sensible heat flux , net radiation flux and photosynthetic active radiation are all significantly positively related with CO2 flux .

森林蒸散量日变化特点是白天高于夜间，中午最高，夜间潜热通量和显热通量（H）有低估的现象；

Forest evapotranspiration was higher in the daytime than that at night , with the highest value occurring at noon .

开花期至蜡熟期，水稻冠层白天总潜热通量FACE比对照平均低6.7%。

From flowering to maturing stage , the average difference of daytime total canopy latent heat flux between ambient and FACE was about 6.7 % .

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 .

潜热通量与CO2通量的相关系数在0.920~0.955之间，苗期、拔节期和抽穗期相关性较高，灌浆期较低；

The correlation coefficient of latent heat flux to CO2 flux is0.920 ~ 0.955 , which is higher in seedling , jointing and heading stages , and lower in filling stage .

热带气旋-海洋相互作用通过SST下降减少向上的热通量，潜热通量的减少对SST的下降更敏感。

Upward heat flux is decreased by SST reduction induced by air-sea interaction , the laten heat flux decrease is more sensitive to the SST reduction .

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 .

关于其机制，本文认为主要是海洋对大气强迫的动力响应导致那里的SST变冷，尽管潜热通量的贡献也很显著。

Regarding the mechanism responsible for this , the ocean dynamical response to the atmospheric forcing is suggested to be active , while the contribution of latent heat flux is also significant .

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 .

利用SiB模式计算了地表辐射。感热、潜热通量，并且预报地表温度。

In the SiB model , we calculated the radiation , sensible heat , latent heat flux and the daily variation of temperature at the surface .

模态二反映了南海地区感热和潜热通量变化与南海ITCZ变化的联系；

Mode 2 presents the relation between the variation of sensible and latent heat fluxes and the variation of South China Sea 's ITCZ .

植被LAI的异常变化主要影响太阳辐射在植被与地表之间的分配，以及地表的感热、潜热通量。

The anomalous change in LAI alters the partitioning of the solar radiation reaching at ground surface between vegetation and soil surface , as well as the sensible and latent heat fluxes of ground surface .

本文利用19701979年COADS2°×2°格点月平均资料，计算了30°S30°N热带太平洋和印度洋洋面上的有效长波辐射、感热和潜热通量以及它们的季节变化和年变化。

2 °× 2 ° mean monthly COADS grid data ( 1970-1979 ) are used to compute the net longwave radiation and fluxes of sensible and latent heat over the tropical Pacific and Indian Ocean ( 30 ° S - 30 ° N ) and their seasonal and annual variations .

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 .

结果表明，在土壤湿度空间分布不均匀的情况下，运用Mosaic方法计算得到的地表潜热通量偏小，背景风较小的时候偏差较大，背景风增强时偏差减小。

The results show that , under the sub-grid heterogeneous distribution of soil moisture , the surface latent heat flux calculated by Mosaic method is smaller than their true values . Moreover , with the background wind increasing , the deviation decreases .

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 .

模态三反映了南海地区感热和潜热通量西北&东南向的半年周期振荡。

Mode 3 presents northwest-southeast swing of sensible and latent heat fluxes .

潜热通量总体上是市区小于郊区。

Latent heat flux in urban is smaller than suburban .

热收支中，潜热通量所占的份额增多；

Share of latent heat flux in the heat budget tends to increase ;

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 .

热带太平洋海域感热、潜热通量的时空特征

Spatial and temporal characteristics of latent and sensible heat flux in Western Pacific Ocean

潜热通量日变化峰值时间与气象要素关系均不显著。

Meteorological factors had no impact on the diurnal centroid for latent heat flux .

潜热通量是地表/大气热量交换的主要分量；

Latent heat fluxes were the main component of land surface / air energy exchanges .

利用卫星遥感资料反演感热和潜热通量的研究综述

Using satellite remotely sensed data to retrieve sensible and latent heat fluxes : a review

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 .

不同时间尺度系统对热带太平洋海-气潜热通量贡献的估计

Estimating contributions of systems with different time scale to latent heat fluxes over tropical Pacific Ocean

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 ;

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 .