物种多样性地理分布格局及其成因是生物地理学和宏观生态学研究的核心问题之一。为了解释物种多样性的分布格局,人们提出了多种假说,其中讨论最多的是能量假说。该假说认为,物种多样性的变化受能量控制。根据能量的不同形式及其对物种...物种多样性地理分布格局及其成因是生物地理学和宏观生态学研究的核心问题之一。为了解释物种多样性的分布格局,人们提出了多种假说,其中讨论最多的是能量假说。该假说认为,物种多样性的变化受能量控制。根据能量的不同形式及其对物种多样性的影响机制,能量假说包括以下几种形式:生产力假说(productivity hypothesis)、水分—能量动态假说(water-energy dynamic hypothesis)、环境能量假说(ambientenergy hypothesis)、寒冷忍耐假说(freezing tolerance hypothesis)以及生态学代谢假说(metabolic theory of ecology,MTE)。本文系统介绍了每种能量假说的含义、所使用的能量形式及表征变量,以及对物种多样性的影响机制,并对不同形式的能量假说进行了比较,在此基础上,分析了每种能量假说的优点和缺点以及各自面临的问题。展开更多
During the mei-yu period,the east edge of the Tibetan Plateau and the Dabie Mountain are two main sources of eastward-moving mesoscale vortices along the mei-yu front(MYF).In this study,an eastward-moving southwest vo...During the mei-yu period,the east edge of the Tibetan Plateau and the Dabie Mountain are two main sources of eastward-moving mesoscale vortices along the mei-yu front(MYF).In this study,an eastward-moving southwest vortex(SWV) and an eastward-moving Dabie vortex(DBV) during the mei-yu period of 2010 have been investigated to clarify the main similarities and differences between them.The synoptic analyses reveal that the SWV and DBV were both located at the lower troposphere;however,the SWV developed in a "from top down" trend,whereas the DBV developed in an opposite way.There were obvious surface closed low centers corresponding to the DBV during its life span,whereas for the SWV,the closed low center only appeared at the mature stage.Cold and warm air intersected intensely after the formation of both the vortices,and the cold advection in the SWV case was stronger than that in the DBV case,whereas the warm advection in the DBV case was more intense than that in the SWV case.The Bay of Bengal and the South China Sea were main moisture sources for the SWV,whereas for the DBV,in addition to the above two moisture sources,the East China Sea was also an important moisture source.The vorticity budget indicates that the convergence was the most important common factor conducive to the formation,development,and maintenance of the SWV and DBV,whereas the conversion from the vertical vorticity to the horizontal one(tilting) was the most important common factor caused the dissipation of both of the vortices.The kinetic energy(KE) budget reveals that the KE generation by the rotational wind was the dominant factor for the enhancement of KE associated with the SWV,whereas for the DBV,the KE transport by the rotational wind was more important than the KE generation.The KE associated with the SWV and the DBV weakened with different mechanisms during the decaying stage.Furthermore,the characteristics of baroclinic and barotropic energy conversions during the life spans of both vortices indicate that the SWV and DBV both belong 展开更多
Energy budgets were analyzed to study the development of an eastward propagating southwest vortex (SWV) associated with heavy rainfall over southern China(11-13 June 2008).The results show that kinetic energy(KE) gene...Energy budgets were analyzed to study the development of an eastward propagating southwest vortex (SWV) associated with heavy rainfall over southern China(11-13 June 2008).The results show that kinetic energy(KE) generation and advection were the most important KE sources,while friction and sub-grid processes were the main KE sinks.There was downward conversion from divergent to rotational wind KE consistent with the downward stretching of SWVs.The Coriolis force was important for the formation and maintenance of the SWV.Convergence was also an important factor for maintenance,as was vertical motion during the mature stage of the SWV and the formation stage of a newly formed vortex(vortex B).The conversion from available potential energy(APE) to KE of divergent wind can lead to strong convection.Vertical motion influenced APE by dynamical and thermal processes which had opposite effects. The variation of APE was related to the heavy rainfall and convection;in this case,vertical motion with direct thermal circulation was the most important way in which APE was released,while latent heat release and vertical temperature advection were important for APE generation.展开更多
文摘物种多样性地理分布格局及其成因是生物地理学和宏观生态学研究的核心问题之一。为了解释物种多样性的分布格局,人们提出了多种假说,其中讨论最多的是能量假说。该假说认为,物种多样性的变化受能量控制。根据能量的不同形式及其对物种多样性的影响机制,能量假说包括以下几种形式:生产力假说(productivity hypothesis)、水分—能量动态假说(water-energy dynamic hypothesis)、环境能量假说(ambientenergy hypothesis)、寒冷忍耐假说(freezing tolerance hypothesis)以及生态学代谢假说(metabolic theory of ecology,MTE)。本文系统介绍了每种能量假说的含义、所使用的能量形式及表征变量,以及对物种多样性的影响机制,并对不同形式的能量假说进行了比较,在此基础上,分析了每种能量假说的优点和缺点以及各自面临的问题。
基金supported by the project of the State Key Laboratory of Severe Weather,Chinese Academy of Meteorological Sciences(Grant No. 2010LASW-A02)National Natural Science Foundation of China(Grant Nos.40930951 and 41040037)+1 种基金Chinese Special Scientific Research Project for Public Interest(Grant No.GYHY200906004)National Key Basic Research and Development Project(Grant No.2010CB951804)
文摘During the mei-yu period,the east edge of the Tibetan Plateau and the Dabie Mountain are two main sources of eastward-moving mesoscale vortices along the mei-yu front(MYF).In this study,an eastward-moving southwest vortex(SWV) and an eastward-moving Dabie vortex(DBV) during the mei-yu period of 2010 have been investigated to clarify the main similarities and differences between them.The synoptic analyses reveal that the SWV and DBV were both located at the lower troposphere;however,the SWV developed in a "from top down" trend,whereas the DBV developed in an opposite way.There were obvious surface closed low centers corresponding to the DBV during its life span,whereas for the SWV,the closed low center only appeared at the mature stage.Cold and warm air intersected intensely after the formation of both the vortices,and the cold advection in the SWV case was stronger than that in the DBV case,whereas the warm advection in the DBV case was more intense than that in the SWV case.The Bay of Bengal and the South China Sea were main moisture sources for the SWV,whereas for the DBV,in addition to the above two moisture sources,the East China Sea was also an important moisture source.The vorticity budget indicates that the convergence was the most important common factor conducive to the formation,development,and maintenance of the SWV and DBV,whereas the conversion from the vertical vorticity to the horizontal one(tilting) was the most important common factor caused the dissipation of both of the vortices.The kinetic energy(KE) budget reveals that the KE generation by the rotational wind was the dominant factor for the enhancement of KE associated with the SWV,whereas for the DBV,the KE transport by the rotational wind was more important than the KE generation.The KE associated with the SWV and the DBV weakened with different mechanisms during the decaying stage.Furthermore,the characteristics of baroclinic and barotropic energy conversions during the life spans of both vortices indicate that the SWV and DBV both belong
基金supported by the project of the State Key Laboratory of Severe Weather,Chinese Academy of Meteorological Sciences (Grant No.2010LASW-A02)National Natural Science Foundation of China(Grant No.40875021)+1 种基金the project of the National Key Basic Research and Development of China(No.2009CB421401)the Chinese Special Scientific Research Project for Public Interest(Grant No. GYHY200906004).
文摘Energy budgets were analyzed to study the development of an eastward propagating southwest vortex (SWV) associated with heavy rainfall over southern China(11-13 June 2008).The results show that kinetic energy(KE) generation and advection were the most important KE sources,while friction and sub-grid processes were the main KE sinks.There was downward conversion from divergent to rotational wind KE consistent with the downward stretching of SWVs.The Coriolis force was important for the formation and maintenance of the SWV.Convergence was also an important factor for maintenance,as was vertical motion during the mature stage of the SWV and the formation stage of a newly formed vortex(vortex B).The conversion from available potential energy(APE) to KE of divergent wind can lead to strong convection.Vertical motion influenced APE by dynamical and thermal processes which had opposite effects. The variation of APE was related to the heavy rainfall and convection;in this case,vertical motion with direct thermal circulation was the most important way in which APE was released,while latent heat release and vertical temperature advection were important for APE generation.
