- 更多网络例句与大气温度相关的网络例句 [注：此内容来源于网络，仅供参考]
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The linear theory of antisymmetric ducted gravity waves supported by mesospheric thermal duct is presented, propagation and evolution of gravity wave packets in thermal duct is also simulated by using a nonlinear two-dimensional model. Numerical results show that lower atmospheric wave disturbance can penetrate into the duct area and be trapped.
给出了重力波在中层大气温度波导中的反对称形式导制传播的线性理论模型，并采用二维非线性的数值模型对重力波波包在中层大气温度波导中的传播和演变过程进行了模拟研究。
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We used NCAR/NCEPT anew analyze data and the method of bilinearity insert to fix on profile distribution of several physical field in the air on observation point and the stream field of 700hPa. We primary discussed the possible mechanism to influence aerosol size distribution.The atmospheric condition of 1000hPa~700hPa level had great influence on aerosol size distribution, and influence on coarse particle mainly below 850hPa level. The horizontal wind velocity of 925hPa level is a primary gene which contributed to coarse particles in the air. Vorticity profile especially below 700hPa level is a key gene to influence diffuse and convergence of local aerosol. The air vertical motion velocity greatly influenced aggregation and remove of aerosol particles. The vertical distribution of air temperature mainly influenced vertical transportation of aerosol.
利用NCAR／NCEP逐日再分析资料，通过双线性插值方法，确定观测点上大气中几个物理量的廓线分布；及700hPa的流场，初步探讨了影响大气中气溶胶粒子谱分布的可能机制： 1000hPa～700hPa的大气状况对气溶胶粒子谱分布影响显著，对粗粒子气溶胶的影响显著的主要集中在850hPa以下；925hPa的水平风速是影响大气中粗粒子气溶胶的一个主要因子；涡度廓线(尤其是700hPa左右及以下的涡度廓线)是影响局地气溶胶的扩散的一个关键因子；大气的垂直运动速度对气溶胶的聚合及移出影响较大；大气温度的垂直分布主要影响气溶胶垂直输送。
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The model is run under the idealized conditions resresenting for the sea-ice diploe in the Okhotsk Sea and the Bering Sea, and the atmospheric forcing is from the data of the winter months i.
参考已有的理论和模拟研究结果，指出高纬地区低空大气的温度变化受直接热力学调整过程的影响明显，对称性响应分量明显，而高层大气温度和各层的大气位势高度变化是由直接热力学调整和间接动力过程响应所共同控制，非对称分量占主导。
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Thats the first problem should be solved for getting a good retrieval. Based on the cognition, a method is developed to assess the retrievability of temperature and the distribution of the global retrievability with HIRS/3 and AIRS data in Jan and Jul are firstly given by using the NCEP reanalysis data. The results show that the retrievability of temperature is low in the upper and lower atmosphere, and high between 400 hPa and 850 hPa.
基于这样的认识，本文首先利用奇异值分解方法结合经验正交分解技术，导出一种计算大气温度可反演度的方法，并利用NCEP再分析资料首次给出了全球1月和7月分别由HIRS/3和AIRS资料反演大气温度廓线时的可反演度分布，结果表明温度的可反演度在高层和低层较小，400hpa—850hpa之间较大。
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Based on the cognition, a method is developed to assess the retrievability of temperature and the distribution of the global retrievability with HIRS/3 and AIRS data in Jan and Jul are firstly given by using the NCEP reanalysis data. The results show that the retrievability of temperature is low in the upper and lower atmosphere, and high between 400 hPa and 850 hPa. In geographical distribution, the retrievabilities are low in the low latitude marine regions and in some regions in Antarctica, and relatively high in mid-high latitude regions and continental regions.
基于这样的认识，本文首先利用奇异值分解方法结合经验正交分解技术，导出一种计算大气温度可反演度的方法，并利用NCEP再分析资料首次给出了全球1月和7月分别由HIRS/3和AIRS资料反演大气温度廓线时的可反演度分布，结果表明温度的可反演度在高层和低层较小，400hpa—850hpa之间较大。
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Based on the systematic observations conducted from 2002 to 2003, the mean temperature characteristics and variation behaviors of the middle atmosphere temperature profiles over Wuhan are given. The limitations of standard atmosphere mode in describing the characteristics of middle atmosphere are discussed.
基于 2 0 0 2年至 2 0 0 3年激光雷达的系统观测数据，给出了武汉上空中层大气温度分布的年平均特性及在各种时间尺度下的变化规律，分析了标准大气模式在描述中层大气温度分布平均特性和变化规律上的局限。
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The main characteristics include: the quiet Sun corona has a rapid response to the flare heating, within 2 second the corona temperature increases nearly one order of magnitude, but later such increase becomes very slowly; the downward velocity at early stage of impulsive phase is too small to be negnected; chromospheric evaporation made by conduction shows some intensely, the maximum evaporated velocity may be as large as 1000 km/s; the chromospheric condensation appears just when the chromospheric evaporation takes place and its place always coincide with that of transition region in the early stage; the maximum of chromospheric condensation occurs also in the early stage of impulsive phase, at which the density in condensation may be larger two order of magnitude than that of surround and the downward velocity may be as large as 100 km/s; after the maximum of chromospheric condensation, its strongth decreases gradually but its width becomes greater with time and have a tendency to transport into deep chromosphere; the front of chromospheric condensation heats atmosphere obviously and the temperature in the chromospheric condensation is higher than the original case; the downware velocity of transition region may be greater than 100 km/s at the early stage; when the evaporated material collide at the top of loop, the densityand the presure there increase rapidly, which result in the formation of a shock wave; and so on.
在改善色球辐射损失和精确分辨过渡区的基础上，通过联立求解连续性方程、动量方程和能量方程，构造了一维磁限制性耀斑环在热沉积作用下的大气动力学模型，获得了耀斑热模型下脉冲相早期较为细致的大气演化理论图象，其主要特征是：耀斑对宁静日冕的加热相当迅速，仅2秒钟日冕温度增加即达一个量级，之后日冕温度增加缓慢；脉冲相早期日冕向下速度很小，几乎可以忽略，热传导驱动色球蒸发，其过程较为激烈，蒸发极大速度可达到1000km/s；色球压缩区与色球蒸发几乎同时形成，且在早期其位置总是与过渡区位置重合；色球压缩极大发生在脉冲相早期，其时密度可高于周围约2个量级，向下速度可超过100km/s；色球压缩极大后，其强度逐渐减弱，但宽度明显增大，且渐渐脱离过渡区往色球传播；压缩区内物质温度要高于原先的大气温度；过渡区下降在脉冲相早期相当迅速，可超过100km/s；当蒸发物质在环顶高速相碰时，环顶的密度、压力迅速增大，且温度也有所增加，导致形成激波，其波面以每秒上百公里的速度自环顶向下传播；在脉冲相前期，日冕软x辐射对色球的加热作用可以忽略；等。
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Three periods are clearly divided based on decadal mean temperatures of the records for global surface temperatures of recent 120 years.
根据近 1 2 0年来全球大气温度的记录，进行了每 1 0年平均气温的分析，可以明显地划分为 3个时期即温度偏低期(1 880～ 1 91 9年，至少 40年)，过渡期(温度变化起伏不大，1 92 0～ 1 979年，约 60年)和升温期。
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A high spectral resolution lidar was used for low level atmospheric temperature measurement. Based on the iodine filter's high absorption property for aerosol, the HSRL retrieves low level atmospheric temperature with Rayleigh backscattering signal intensity.
基于碘分子滤波器对大气气溶胶散射的强吸收特性，滤除低层大气中气溶胶散射的影响，从而利用分子瑞利后向散射信号强度反演低层大气温度。
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The trail bridge design,the mixture performance test,the temperature between the different layers of the deck surfacing,the traffic investigation and the surface performance observation are introduced in this article.The basic performance of the mixture used in the trial bridge is analyzed through rutting tests at high temperature,bending tests at low temperature,fatigue tests of the composite beam and pull off tests.The rule of the temperature gradient distribution in the pavement and the variety relation ...
介绍润扬大桥钢桥面铺装试验桥的方案设计、试验研究、温度测试、交通量调查和使用性能跟踪观测，通过混合料高温车辙试验、低温弯曲试验、复合梁疲劳试验以及拉拔试验等分析实桥试验沥青混合料基本性能，阐述铺装内各层温度梯度分布规律及与大气温度变化关系，通过使用性能跟踪观测介绍浇注式沥青混凝土+环氧沥青混凝土新型铺装结构的工程效果。
- 更多网络解释与大气温度相关的网络解释 [注：此内容来源于网络，仅供参考]
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air temperature：气温
[简介]气温(air temperature) 通常人们用大气温度数值的大小,反映大气的冷热程度. 大气的温度简称气温,我国用摄氏温标,以℃表示,读做摄氏度. 人们根据水银(酒精)热胀冷缩的原理发明了温度计,并将其安装在特殊的装置内,对气温进行自动连续监测.
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dew point：露点[温度]
露点温度(Dew Point)是一个描述大气中水凝结的一个参数,其定义是固定大气压下,空气中所含的水汽达到饱和而凝结时的温度,一般地,露点要比温度值低. 当大气相对湿度为100%时,露点温度等于大气温度.
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atmospheric electricity：天电,大气电
Asymptotic stability 渐近稳定性 | Atmospheric electricity 天电,大气电 | Atmospheric moisture 大气温度
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oat：外界大气温度
P 外界大气温度(OAT)P 外界大气温度(OAT)AP1就是类似于默认的AP电门,AP2允许您使用空速(IAS)/马赫数(MACH)方式爬升和高度保持方式
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atmospheric shimmer：大气闪烁
"大气散射","atmospheric scattering" | "大气闪烁","atmospheric shimmer" | "大气温度","atmospheric temperature"
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atmospheric shimmer：大气内铄
大气圈 atmospheric shell | 大气内铄 atmospheric shimmer | 大气温度 atmospheric temperature
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TREF Flat Rating Temperature：平推力温度
TISA Standard temperature 标准大气温度 | TREF Flat Rating Temperature 平推力温度 | T/C Top of Climb 爬升顶点
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atmospheric temperatures：大气温度
atmospheric concentrations of carbon dioxide 大气中的二氧化碳浓度 | atmospheric temperatures 大气温度 | attributable adj. 可归于...的
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atmospheric temperatures：大气温度CHA中国英语学习网
atmospheric concentrations of carbon dioxide 大气中的二氧化碳浓度CHA中国英语学习网 | atmospheric temperatures 大气温度CHA中国英语学习网 | attributable adj. 可归于...的CHA中国英语学习网
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dewpoint：露点温度
outside air temperature 外界温度,大气温度 | dewpoint 露点温度 | the temperature rise 温度上升