夏季东亚副热带反气旋进退活动的非线性机理讨论

采用三维强迫耗散非线性动力学模式,结合夏季东亚副热带地区实际的环流结构和天气特征,对东亚上空副热带反气旋的活动进行了研究和探讨,导出了系统稳定性的位涡拟能判据并据此进行了分析和讨论·所得判据可为分析和预报夏季东亚上空副热带高压的进退变化及相应的东亚天气提供参考依据·     

一种新的海面空气动力学粗糙度方案

综合利用6个国际海洋观测试验资料,共同验证Charnock参数与无因次粗糙度长度(z0/Hs)对波龄的依赖性,建立粗糙度回归模型,并对其进行显著性和适用性检验,从而导出粗糙度无因子形式与有效波高有关.利用研制的粗糙度方案(SP07)研究充分发展风浪与风区、风时和水深的关系,及粗糙度长度对摩擦速度和波龄的敏感度.把SP07方案引人国际上最先进的计算海气通量的COARE(V3.0)算法中,选择1985年12月在北海的FPN平台上的试验资料,进一步检验SP07方案的适用性.得出目前国际上最先进的002和TY01方案较高估计了摩擦速度,YT96方案略偏低估计了摩擦速度,文中研制的方案计算结果与实测结果最接近.     

Soliton-like thermal source forcing and singular response of atmosphere and oceans to it

IntroductionAsystemfrequentlyobservedingeophysicalfluidsthatislong_lived ,organized ,andalwaysofsteadylarge_amplitudeiscalledasolitonasaphenomenonwhichisseen ,forexample,asa“greatspot”intheJupiter’satmosphereandablockinghigh’ssituationintheatmosphereofourplanetary[1].Inthenonlinearforcing_dissipativesystemsoftheatmosphereandoceansthesolitonisbothaspecialandanessentialentity .Onadynamicbasis,itcanbeviewedapproximatelyasaproductwhenbalanceisreachedbetweenlineardispersionandnonlinearsteepness…     

孤立子型热源强迫与大气和海洋流场的奇异响应

运用非线性动力学分析方法,对一个广义的地球流体动力学正压准地转模式中,局地热源强迫对大气和海洋流场产生的响应结果,进行了解析研究.发现热源扰动和响应流场之间存在很好的对应关系:两者具有类似的分布模态,且孤立子型的响应流场要比孤立子型的热源强迫范围大得多,即"狭窄"的热源扰动可能导致"宽广"的流场响应;强迫热源的特殊结构有可能导致大气或海洋流场出现奇异响应,从而使大气或海洋环流发生异常(如大气阻塞现象);中、高纬地区的大气和海洋流场对热源强迫的响应要比低纬地区显著得多.上述结果与中、低纬大气试验和观测资料的研究结果相符,可部分解释地球流体中,局地热源异常可能导致的环流异常现象.     

A discussion of non-linear mechanism on subtropical anticyclone's extending/shrinking over East-Asia in summer

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A preliminary study on sea wave packet equations on slowly varying topography

There is a common hypothesis for the presently popular mild-slope equations that wave particle motion is irrotational. In this paper, an attempt is made to abandon the irrotational assumption and to set up new sea wave packet equations on slowly varying topography by use of the WKBJ method. To simplify the deduction, the two-dimensional shallow water equations are used to describe the sea wave particle motion in the very shallow nearshore area. The established equations can give some characteristics of wave propagation near shore.