Sensible Heat Flux

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

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。

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 .

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。

An Improved Regional Scale Sensible Heat Flux Model Using Remote Sensing

基于卫星遥感数据改进区域尺度的显热通量模型

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

亚洲季风区地面感热通量的区域变化特征

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

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 mesoscale sensible heat flux is influenced by many facts .

而中尺度感热通量的强弱受多种因素的制约。

A Diagnostic Study of Surface Sensible Heat Flux Anomaly over the Qinghai-Xizang Plateau

青藏高原地面感热及其异常的诊断分析

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

绿洲地区感热通量小，潜热通量大；

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

热带太平洋海域感热、潜热通量的时空特征

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

风向对LAS和EC观测感热通量值有显著影响。

The peak value of latent heat flux was higher than that of sensible heat flux in summer .

在夏季，农田和森林的潜热通量的峰值大于感热通量。

Simulating Diagnostic Analyses for Frontogenesis and Surface Sensible Heat Flux of a Sand-Dust Storm Process

一次沙尘暴过程锋生函数和地表热通量的数值诊断

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

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 very greater than the latent heat flux in the PBL air .

地表感热通量明显大于地表潜热通量；

Relationships of sensible heat flux , latent heat flux and momentum fluxes with meteorological elements are different .

通量变化受不同环境要素的影响：感热通量与海-气温差呈正相关关系，与气温呈明显的负相关关系。

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

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。

Long-term analysis : The sensible heat flux and the latent heat flux reanalysis data were bigger than their observed data .

长期分析发现：感、潜热通量再分析数据比对应的实测数据偏大。

Sensible heat flux was up to 50 % of net radiation and generally reached 80 % ~ 100 % .

白天，感热通量占净辐射的50%以上，一般达80%～100%。

The results show that the ratio of the latent heat flux to the sensible heat flux is10.14 ;

指出西大平洋暖池海区游热通量与显效通量之比为10.14：1；

In dry seasons , the energy change was mainly caused by increasing albedo , leading to sensible heat flux decreased .

在旱季，能量平衡的变化主要是由于地表反照率增大造成净短波辐射和地表感热通量减小；在雨季，由于大面积森林砍伐造成植被蒸腾作用减小，地表蒸散减小，潜热通量也相应减小。

Temporal and Spatial Patterns of Surface Sensible Heat Flux and Their Relationship with the SST Anomaly over Adjacent Oceans

地表感热的时空分布特征及其与邻近海洋海温异常的关系

The sensible heat flux is dominant in the heat energy budget on ground surface and the latent heat can be neglected .

这时在地表面热量平衡过程中，潜热可以忽略不计，感热占绝对优势。

In this area , the short wave radiation accepted by the surface is mainly released by sensible heat flux and long wave radiation .

陆面所接收的太阳短波辐射主要以感热和长波辐射的能量形式释放。

The reaction of SST and sensible heat flux responding to abnormal latent heat flux curbs this positive feedback process .

在潜热通量与大气相互作用的正反馈机制中，海温和感热通量的响应对这种正反馈过程起到一定的抑制作用。

All the component changes of sensible heat flux and latent heat flux are related to the wet and dry & season changes .

显热通量、潜热通量等分量的变化都与干湿季节变化有关，潜热消耗热量是显热消耗热量的6.9倍。

The sensible heat flux decreased by 52.6 % , 11.1 % in a clear and overcast daytime respectively ;

晴天和阴天间作系统的感热通量均低于单作系统，分别约低52.6%和11.1%；

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

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。

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

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。

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

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。

Urban canyon is the main source of urban sensible heat flux . Thus , urban canyon can not be neglected in the urban weather research .

城市峡谷是城市感热通量的主要来源，因此，在研究城市气象时不能忽略城市峡谷的影响。