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771.
青藏高原地区云对地面有效辐射的影响:Ⅱ.强迫作用 总被引:2,自引:0,他引:2
本文利用1982年8月-1983年7月青藏高原地面热源观测试验资料,讨论了与云对地面有效辐射强迫作用有关的参数的计算问题,并对这些参数的计算结果进行了分析。结果表明:晴空、全云条件下的地面有效辐射和云对地面有效辐射强迫作用的年平均日变化振幅有明显的地域差异;云对地面有效辐射的强迫作用春夏大,秋冬小,甘孜、拉萨、那曲和改则4站平均的年平均值为-27.2W/m^2。? 相似文献
772.
Qi Zhang Jiquan Zhang Denghua Yan Yongfang Wang 《Theoretical and Applied Climatology》2014,117(1-2):169-174
Extreme weather events include unusual, severe or unseasonal weather, and weather at the extremes of the historical distribution. They have become more frequent and intense under global warming, especially in mid-latitude areas. They bring about great agricultural and economic losses. It is important to define the threshold of extreme weather event because it is the starting point of extreme weather event research, though it has been of seldom concern. Taking extreme precipitation events in Anhui, China as an example, the detrended fluctuation analysis (DFA) method is introduced to define the threshold of extreme weather events. Based on it, the spatial and temporal distributions of extreme precipitation events are analyzed. Compared to the traditional percentile method, DFA is based on the long-term correlation of time series. Thresholds calculated by DFA are much higher than the 99th percentile and the values are higher in the south and lower in the north. This spatial pattern is similar to the annual precipitation spatial pattern. There is an obvious increasing trend in the number of days with extreme precipitation, especially after the 1980s. This observation supports the point that more extreme events happen under global warming. 相似文献
773.
以厦门市旅游业为研究样本,采用系统分析,围绕气候变化对旅游业发展的影响,建立气候变化对旅游业发展影响的评价指标体系,利用层次分析法对各指标因子进行权重测算,再利用模糊综合评价法进行评价,将气候变化对厦门旅游业的影响进行定量分析。结果显示,气候变化对旅游业的影响的隶属度最大值为0.309,是较强的。研究可以明确将旅游业发展过程中受气候变化影响的各个方面,按照受影响程度高低进行划分,从而可以有效指导旅游业相关从业者对风险进行归类,进而协调各方利益,有针对性地发展旅游业,从而实现旅游资源的长期利用和旅游业的可持续发展。 相似文献
774.
Shanghai experienced the longest rainy days in 2018/2019 winter since 1988. The physical cause of such an unusual climate condition was investigated through the diagnosis of observational data. From a seasonal perspective, a long persistent rainy winter was often associated with an El Niño condition in the equatorial Pacific. This abnormal oceanic condition induces a remote teleconnection pattern with pronounced low-level southerly anomalies over East China. The wind anomalies transported moisture from tropical oceans and caused persistent rainfall in East Asia. Meanwhile, the local rainfall time series exhibited a strong quasi-biweekly oscillation (QBWO). Three persistent rainy events were identified in the 2018/2019 winter and they all occurred during the active phase of the QBWO. The first two events were associated with a low pressure anomaly west of Shanghai. Southerly anomalies associated with the low pressure system advected high mean moisture into central eastern China, leading to the persistent rainfall there. The third event was associated with a high pressure anomaly in lower troposphere to the east of Shanghai, which induced anomalous southerlies to its west, favoring the occurrence of rainfall in Shanghai. The result suggests the importance of high-frequency variability in affecting seasonal rainfall anomalies. 相似文献
775.
In this paper, lead-time and spatial dependence in skill for prediction of monthly mean climate variability is analyzed. The analysis is based on a set of extensive hindcasts from the Climate Forecast System at the National Centers for Environmental Prediction. The skill characteristics of initialized predictions is also compared with the AMIP simulations forced with the observed sea surface temperature (SST) to quantify the role of initial versus boundary conditions in the prediction of monthly means. The analysis is for prediction of monthly mean SST, precipitation, and 200-hPa height. The results show a rapid decay in skill with lead time for the atmospheric variables in the extratropical latitudes. Further, after a lead-time of approximately 30?C40?days, the skill of monthly mean prediction is essentially a boundary forced problem, with SST anomalies in the tropical central/eastern Pacific playing a dominant role. Because of the larger contribution from the atmospheric internal variability to monthly time-averages (compared to seasonal averages), skill for monthly mean prediction associated with boundary forcing is also lower. The analysis indicates that the prospects of skillful prediction of monthly means may remain a challenging problem, and may be limited by inherent limits in predictability. 相似文献
776.
777.
利用鲁西南地区雾日与同期、前期全球500hPa高度资料,统计得出欧亚大陆槽脊位置,亚洲南北两支锋区的位置、强度、走向等与鲁西南地区雾日密切相关,并选取优势因子建立鲁西南地区月、旬、候雾日预测方程,试报结果表明,用前期全球500hPa高度资料预测雾日具有一定的效果。 相似文献
778.
779.
In this paper, a nonlinear optimization method is used to explore the finite-time instability of the atmospheric circulation
with a three-level quasigeostrophic model under the framework of the conditional nonlinear optimal perturbation (CNOP). As
a natural generalization of linear singular vector (SV), CNOP is defined as an initial perturbation that makes the cost function
the maximum at a prescribed forecast time under certain physical constraint conditions. Special attentions are paid to the
different structures and energy evolutions of the optimal perturbations. 相似文献
780.
甘肃中川地区雷暴地闪特征的初步分析 总被引:4,自引:5,他引:4
本文分析了1987年6月28日甘肃中川地区一次雷暴过程中地面4个测站的电场资料,并定量估算了4个地闪的8个回击所中和的电荷量及其高度。负地闪回击所中和的电荷离地高度为4km左右(对应的环境温度为-11.2℃),而正地闪回击所中和的电荷离地高度为2km左右(环境温度+4.9℃)。负地闪大多发生在云闪后的电场恢复阶段,且在开始时往往具有持续几百毫秒的云内放电过程。其激发过程可能是首先在云底部正电荷区产生向上传输的持续正流光,导致云中部负电荷向下移动,并引发向下传输的负先导,最终导致地闪回击的发生。 相似文献