By using the rawinsonde data, upper cloud amount data and objective analysis data for global domain which all were produced by Numerical Prediction Division,JMA and by using daily and mean weather map issUed by JMA an...By using the rawinsonde data, upper cloud amount data and objective analysis data for global domain which all were produced by Numerical Prediction Division,JMA and by using daily and mean weather map issUed by JMA and daily rainfall data over the Huaihe River Basin from China,an observational study to the early summer seasonal change of large-scale circulation over East Asia and its relation to change of the frontal features and environment for the frontal rainfall has been carried out.Following reaults have been obtained:(1) The early summer seasonal change of large-scale circulation was occurred during 20-23 May 1991,which was about 10 days earlier than the normal.During the period the subtropical westerly jet and tropical easterlies abruptly moved northward;(2) The northward movement of the tropical easterlies was not uniform,it was earlier at 100 hpa level and about 24 hrs late at 200 hpa level.The phenomenon was associated with earlier disappearence of the subtropical westerly jet at 100 hpa level;(3)During the seasonal change there were two westerly jets in the upper level and changed their intensity with the time.before 18 May 1991,the southern one was more intense and then changed to more intense for the northern one and disappearence of the southern one,the phenomenon seemed to be appeared as northward movement of the southernjet;(4) A faster temperature(n rising in the upper level over the Tibetan Plateau was associated with the seasonalchange.From the T rising the T maximum moved onto the plateau,changing the T gradient from positive to negahve to the south flank of the plateau,the effect to leduce and disappear the southern westerlies.Also the T rising was associated with change of the frontal features over East Asia;(5) The seasonal change type during 1991 was same as that during 1992 and 1993,but different from that during 1990;(6) The environment for the frontal rainfall was change in the season,the differences were in the baroclinity in upper level and vertical wind speed and direction shear.展开更多
全球气候变暖和大气CO_(2)浓度(Ca)急剧上升已成为不争的事实,并对森林生态系统有着深远的影响,全面理解森林生态系统对全球变化的响应至关重要。中亚干旱区特有树种雪岭云杉(Picea schrenkiana Fisch. et Mey)树轮稳定碳同位素(δ^(13...全球气候变暖和大气CO_(2)浓度(Ca)急剧上升已成为不争的事实,并对森林生态系统有着深远的影响,全面理解森林生态系统对全球变化的响应至关重要。中亚干旱区特有树种雪岭云杉(Picea schrenkiana Fisch. et Mey)树轮稳定碳同位素(δ^(13)C)和水分利用效率(iWUE)对气候变暖和大气CO2浓度急剧上升的响应缺乏研究。本研究利用天山西部伊犁河流域的雪岭云杉树轮样本,使用树木年代学方法和树轮稳定碳同位素技术,建立树轮宽度年表、稳定碳同位素(δ^(13)C)以及内禀水分利用效率(iWUE)序列,分析了树轮δ13C和iWUE的长期变化特征,探讨了树轮δ13C和iWUE对气候的响应规律以及iWUE与树轮宽度的关系。结果表明,主要的气候因子并没有强烈地限制树木径向生长;夏季平均气温对树轮δ^(13)C分馏有重要影响,iWUE的长期变化受到全球Ca增加和升温趋势影响,但直接影响iWUE年际变化的主要因素是饱和水汽压亏缺(VPD)。全球升温和Ca增加导致了iWUE的持续升高,但并没有导致雪岭云杉树木径向生长的明显增加。展开更多
文摘By using the rawinsonde data, upper cloud amount data and objective analysis data for global domain which all were produced by Numerical Prediction Division,JMA and by using daily and mean weather map issUed by JMA and daily rainfall data over the Huaihe River Basin from China,an observational study to the early summer seasonal change of large-scale circulation over East Asia and its relation to change of the frontal features and environment for the frontal rainfall has been carried out.Following reaults have been obtained:(1) The early summer seasonal change of large-scale circulation was occurred during 20-23 May 1991,which was about 10 days earlier than the normal.During the period the subtropical westerly jet and tropical easterlies abruptly moved northward;(2) The northward movement of the tropical easterlies was not uniform,it was earlier at 100 hpa level and about 24 hrs late at 200 hpa level.The phenomenon was associated with earlier disappearence of the subtropical westerly jet at 100 hpa level;(3)During the seasonal change there were two westerly jets in the upper level and changed their intensity with the time.before 18 May 1991,the southern one was more intense and then changed to more intense for the northern one and disappearence of the southern one,the phenomenon seemed to be appeared as northward movement of the southernjet;(4) A faster temperature(n rising in the upper level over the Tibetan Plateau was associated with the seasonalchange.From the T rising the T maximum moved onto the plateau,changing the T gradient from positive to negahve to the south flank of the plateau,the effect to leduce and disappear the southern westerlies.Also the T rising was associated with change of the frontal features over East Asia;(5) The seasonal change type during 1991 was same as that during 1992 and 1993,but different from that during 1990;(6) The environment for the frontal rainfall was change in the season,the differences were in the baroclinity in upper level and vertical wind speed and direction shear.
文摘全球气候变暖和大气CO_(2)浓度(Ca)急剧上升已成为不争的事实,并对森林生态系统有着深远的影响,全面理解森林生态系统对全球变化的响应至关重要。中亚干旱区特有树种雪岭云杉(Picea schrenkiana Fisch. et Mey)树轮稳定碳同位素(δ^(13)C)和水分利用效率(iWUE)对气候变暖和大气CO2浓度急剧上升的响应缺乏研究。本研究利用天山西部伊犁河流域的雪岭云杉树轮样本,使用树木年代学方法和树轮稳定碳同位素技术,建立树轮宽度年表、稳定碳同位素(δ^(13)C)以及内禀水分利用效率(iWUE)序列,分析了树轮δ13C和iWUE的长期变化特征,探讨了树轮δ13C和iWUE对气候的响应规律以及iWUE与树轮宽度的关系。结果表明,主要的气候因子并没有强烈地限制树木径向生长;夏季平均气温对树轮δ^(13)C分馏有重要影响,iWUE的长期变化受到全球Ca增加和升温趋势影响,但直接影响iWUE年际变化的主要因素是饱和水汽压亏缺(VPD)。全球升温和Ca增加导致了iWUE的持续升高,但并没有导致雪岭云杉树木径向生长的明显增加。
