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61.
The NCEP/NCAR II daily mean reanalysis data and observed precipitation data are employed to
investigate the westward extension of the western Pacific subtropical high (WPSH) during the heavy rain
period over the southern China in June 2005. Results show that there may exist a relationship between the
east-west shift of the WPSH and the process of a southern China heavy rain. The analysis indicates that the
vertical motion in the WPSH area is mainly caused by the latent heat release of monsoon rain belts on its
northern and southern sides. The vertical motion could cause the accumulation of air mass in the center
and west of the WPSH, which leads to its strengthening. The appearance of the northern and southern
monsoon rain belts could not only enhance the WPSH by strengthening the descending draft, but also
excite the development of positive vorticity and restrict the WPSH’s movement in the north–south
direction. Moreover, the Indian monsoon rainfall to the west of the WPSH may excite the development of
anticyclonic vorticity on its eastern side, which leads to the westward extension of the WPSH. 相似文献
62.
Based on the temperature of the black body (TBB), station observed and NCEP reanalysis data, the impacts of the eastward propagation of convective cloud systems over the Tibetan Plateau on the southwest vortex (SWV) formation that occurred at 1800 UTC on 29 June 2003 are analyzed by using the Zwack-Okossi (Z-O) equation to diagnose the thermal and dynamic processes. It is found that, in summer, severe convective activities often occur over the Tibetan Plateau due to the abundant supply of moisture. The convective cloud near the east edge of the plateau could move eastward with a short-wave trough in the westerly. The divergent center that is induced by latent heat release, which is associated with severe convective activities, moves out with the convective cloud and contributes to the low level decompression which is favorable for the formation of plateau edge cyclogenesis (PEC). The Z-O equation indicates that, in this case, the latent heat release and convergence are the two most important factors for SWV formation, which amounts to about 42% and 15% of the term TOTAL, respectively. It is implied that the thermal process effect was more important than the dynamic process during SWV formation. 相似文献
63.
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65.
本文利用“中美热带西太平洋海气相互作用研究”第1-8航次海面气象观测资料,计算分析了热带太平洋感热潜热通量的时空特征.分析结果表明在赤道海域,潜热通量远远大于感热通量.潜热和感热通量是从海面向大气输送的,且具有明显的年际变化和季节变化,日变化变幅甚小. 相似文献
66.
盐生荒漠地表水、热与CO2输送 的实验研究 总被引:5,自引:0,他引:5
利用安装在准噶尔盆地南缘多汁盐柴类荒漠上的涡度相关系统与配套的微气象观测系统所得数据,分析了显热、潜热与CO2通量的日过程和季节变化特点及各通量间的相互关系。数据显示了一个明显违背植物水分关系一般规律的现象:当水汽(潜热) 通量明确显示土壤水分亏缺时,净光合(CO2通量) 却未受到影响。因此推测当地原生植物的根系在积盐严重的土壤上层没有发育,所以其水分状况与光合能力不受上层土壤干湿的影响,观测到的水汽通量的变化主要由土壤蒸发的变化造成的。 相似文献
67.
亚洲季风区感热凝结潜热对副高带季节演变的影响 总被引:5,自引:3,他引:5
利用1958-1998年NCEP/NCAR的逐日再分析资料,探讨了亚洲夏季风建立期间感热、凝结潜热和副高带季节演变的气候特征,并重点分析它们相互耦合的特征。结果表明:亚洲季风区的地表感热、凝结潜热影响印缅槽生成和阿拉伯副高西移的机制是相似的,5月初,印度半岛较强的感热通量和中南半岛较强的凝结潜热共同影响副高带的断裂及印缅槽的生成,5月底-6月上旬阿拉伯半岛较大的感热通量和印度半岛西侧较强的凝结潜热有利于阿拉伯副高的西移。 相似文献
68.
The gradient of CO2 concentration, photosynthetically active radiation(PAR). net radiation.soil heat flux, profiles of wind speed, and air temperature and humidity were measured above a wheat field during May and June 1985 at Beijing Agro-Ecosystems Experimental Station. Beijing,China. Fluxes of carbon dioxide, sensible heat, latent heat and momentum were calculated by using the aerodynamic method. The observation site. equipment, calibration techniques, the errors associated with the measurement, and the computational procedures are described. The results show that the diurnal variations of amplitude of CO2 concentrations were 103.8 to 27. 0.86. 3 to 22.8 and 69.8 to 11.6 ppm:the average CO2 concentrations were 331.5. 339.9 and 364.6 ppm for the photosynthesis type, and 369.6. 364.0 and 375.2 ppm for the respiration type at 1. 2 and 10 m above surface, respectively, from May 14 to June 15. In the daytime, transfer direction of the CO2 fluxes and gradients is from air to crop canopy, and at noon(1100 to 1300 BT(Beijing Time)) the transfer rate reaches negative maximum value. At night, transfer of CO2 fluxes and gradients is in the reversed direction and reaches positive maximum in the early morning(0400 to 0600 BT). There are strong negative correlations between CO2 flux and the net radiation(Rn),available energy(H+LE). photosynthetically active radiation(PAR) and momentum flux(τ). 相似文献
69.
本文提出了潜导水的概念,并通过对潜导水主要特征、潜导水压传递原理、潜导水压大小的分析,阐述了潜导水在地下工程洞体突水中的作用。 相似文献
70.
农田近地面层CO2和湍流通量特征研究 总被引:11,自引:0,他引:11
利用1985年5月至6月在北京郊区中国科学院农业生态试验研究站的麦田中实测的小麦不同生长期的CO2浓度梯度、光合有效辐射、净辐射、土壤热通量和温度、湿度及风速梯度等量的数据,采用空气动力学方法,计算了CO2通量、感热通量、潜热通量和动量通量。并对观测场地、仪器设备、校准方法及误差分析进行了描述。结果表明:从5月14日到6月15日,在1m,2m和10m处,CO2浓度振幅的日变化分别为103.4到27.5,87.5到27.3和69.8到11.5ppm;光合型和呼吸型的平均CO2浓度分别为345.3,350.6,357.5ppm和373.9,369.7,362.1ppm。在白天,CO2通量和梯度的输送方向是从大气向植被,在中午(11时到13时)输送达到负的最大值。在夜间,CO2通量和梯度输送的方向与白天相反,并且,在早晨(4时到6时)达到正的最大值。CO2通量与净辐射(Rn)、可利用能(H+LE)、光合有效辐射和动量通量之间有较好的相关关系 相似文献