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221.
In order to investigate the effect of the factors in tower latitudes on Meiyu/Baiu front,adiagnostic analysis for the two cases during June to July of 1985 and 1986 was examined.We foundthat (1)when the tropical convective activity moves westward to 10.5-15.5′N/140°E from eastside of 10.5-15.5°N/160°E,the northward shifts of the Meiyu/Baiu rain belt occurs;(2)themain factor which results in the northward and southward shifts of Meiyu/Baiu rain belt is thoughtas the 8,18 and 30 day oscillations of the tropical convective activity around West Pacific.Meanwhile,the wave train propagating from Lake Baikal via Okhotsk Sea to the tropics couldsometimes shift Baiu rain belt southward;(3)the onsets of Meiyu in China of both cases tend totake place just when the convective activity around lower latitudes moves westward through about140°E with the 8,18 and 30 day oscillation periods firstly coming to June. 相似文献
222.
REGIONAL DIFFERENCES OF TEMPORAL-SPATIAL CHARACTERISTICS OF AIR-SEA INTERACTIONS IN TROPICAL OCEANS 总被引:3,自引:0,他引:3
The singular value decomposition (SVD) of air-sea interaction in the tropical western,central,and eastern Pacific,and the tropical Atlantic and Indian Oceans has been conducted by using theNCEP/NCAR 40-year reanalysis 1000 hPa monthly wind field and COADS monthly sea surfacetemperature (SST).Comparisons of the results suggest that these areas can be divided into threetypes from the viewpoint of air-sea interaction:tropical central-eastern Pacific belongs to monistictype,in which ENSO is the sole important process;tropical western Pacific and Indian Oceansbelong to dualistic type,in which in addition to ENSO.there should be an another importantprocess;tropical Atlantic Ocean belongs to pluralistic type,in which the process is complicatedand the ENSO cycle is not evident. 相似文献
223.
The paper gives the distributions of the daily mean temperature of black body of satellite infrared
images from June 7 to 10, 1998 during HUAMEX and examines 14 meso-α-scale convective systems and a
number of meso-b-scale convective systems using the satellite infrared images at 1-h intervals. The mesoscale
convective systems on June 7 and 9, which resulted in severe rainstorm over the middle of Taiwan and the
estuary region of the Pearl River (Zhujiang R.), are emphatically analyzed. The serial development of mesoscale
convective systems is revealed by the distributions of the black body temperature of satellite infrared images. The
environmental conditions in which many mesoscale convective systems continuously occurred are diagnosed.
The visualizing tool, LiveView, displays the link between the upper and lower horizontal wind fields and the
vertical circulations and 3-dimensional trajectories of moist air motions, based on the data of objective analyses. 相似文献
224.
The trigonometric relationship between slope inclination, the horizontally acting time‐averaged traction force and the vertical depth of transport allows the estimation of one factor, when both others are known. Depth–transport functions can be deduced by comparing the depth distributions of living organisms and their skeletal remains, and this paper simplifies this comparison using foraminifera in which a single test represents an individual. Differences in distribution parameters between living individuals and empty tests allow depth–transport functions to be determined; these functions differ between species at a single transect according to the varying buoyancies of the tests. Within a single species, differences in depth–transport functions between locations are based on either slope inclination or traction intensities. After establishing a mean depth–transport function by averaging species‐characteristic functions, the time‐averaged traction force acting on the studied transect can be calculated. Transport intensities are also estimated using an erosion–deposition diagram that combines the relative frequency distributions of living individuals and empty tests. The proportion of ‘eroded’, ‘parautochthonous’ and ‘allochthonous’ tests mirrors the influence of both slope inclination and traction force for the deposition of empty tests. To test the model, six species of symbiont‐bearing benthic foraminifers were investigated at two transects in front of a NW Pacific coral reef. One transect is distinguished by a strong slope flattening below the steep reef slope (30 m), whereas further steepening characterizes the equivalent part in the other transect. These differences are mirrored in the depth–transport functions as well as in the erosion–deposition diagrams of all species. The time‐averaged traction forces differ in intensities between transects, because of the position of the reef front with respect to the predominant wind direction. However, the form of the functions is identical and distinguished by an increase from the surface to 35 m depth, followed by a decrease down to 105 m. This can be explained by successive onshore and offshore forces acting on the shallow slope, such as the tropical cyclones that cross the region every summer. 相似文献
226.
9403强热带风暴致洪暴雨Tbb特征分析 总被引:2,自引:1,他引:2
本文利用1经纬度间隔Tbb资料分析1994年6月9-10日皖、赣致洪暴雨过程的成因。结果指出,登陆北上的9403强热带低压同西风带降水系统相互作用造成了这场大暴雨过程。南北低值系统的叠置使降水系统结构发生变化,在两云系统接合处产生强对流云团,导致降雨量陡增。分析还表明这场致洪暴雨的发生与下面三个因素有关;1.南、北两云系统都有相当尺度和强度;2.南来云团来自ITCZ和西南地区云系的水源补充;3.不 相似文献
227.
228.
Loreto Donoso Rodrigo Romero Alberto Rondón Emmanuel Fernandez Pedro Oyola Eugenio Sanhueza 《Journal of Atmospheric Chemistry》1996,25(2):201-214
The levels of low molecular weight hydrocarbons were measured at pristine sites and rural locations affected by hydrocarbon emissions from oil and gas producing fields in Venezuela. At the clean sites, lower concentrations of C2 to C6 alkanes were observed, whereas, in comparison with remotes sites, very much higher levels were measured at the polluted sites. Alkenes present relatively high concentrations, with isoprene being the most abundant, all over the study region. The main sources of alkenes are likely to be natural, mainly from vegetation. The levels of alkanes recorded at the clean sites and the alkene levels found everywhere in the region are in agreement with the values reported for other clean sites in the tropics. The increase of ozone production capacity due to the anthropogenic emissions of alkanes from oil and gas fields was estimated. Due to the presence in the atmosphere of important amounts of naturally emitted isoprene, ethene and propene, which makes a substantial contribution to the reactivity of the hydrocarbon mixture, a small increase (<5%) was estimated to occur in the capacity of the ozone production at a regional scale during the rainy season. 相似文献
229.
El Ni?o影响热带大气季节内振荡的动力学研究 总被引:3,自引:0,他引:3
根据El Ni?o期间热带大气状态的异常特征,确定了在简单大气动力模式中描写海温异常的参数化方法。然后利用斜压半地转两层模式从动力学上分析研究了El Ni?o对热带大气低频波的影响。理论分析同有关热带大气季节内振荡的资料分析结果完全一致,El Ni?o事件使热带大气季节内振荡减弱。 相似文献
230.
通过对逐步逼近法1995年试验情况与国内外预报台的综合预报以及与国内一些客观预报方法的比较分析,总结出该方法对移动路径明显转折的热带气旋有较好的预报能力,48小时平均误差达到300km以内,特别是当热带气旋的移速发生明显变化时,该方法较之其它客观方法有明显的优越性。 相似文献