Model simulation output data (CCSM3) related to uplift of Africa and Himalaya/Tibet Plateau and the influence on tropical African vegetation

Hominid evolution in the late Miocene has long been hypothesized to be linked to the retreat of the tropical rainforest in Africa. One cause for the climatic and vegetation change often considered was uplift of Africa, but also uplift of the Himalaya and the Tibetan Plateau was suggested to have impacted rainfall distribution over Africa. Recent proxy data suggest that in East Africa open grassland habitats were available to the common ancestors of hominins and apes long before their divergence and do not find evidence for a closed rainforest in the late Miocene. We used the coupled global general circulation model CCSM3 including an interactively coupled dynamic vegetation module to investigate the impact of topography on African hydro-climate and vegetation. We performed sensitivity experiments altering elevations of the Himalaya and the Tibetan Plateau as well as of East and Southern Africa. The simulations confirm the dominant impact of African topography for climate and vegetation development of the African tropics. Only a weak influence of prescribed Asian uplift on African climate could be detected. The model simulations show that rainforest coverage of Central Africa is strongly determined by the presence of elevated African topography. In East Africa, despite wetter conditions with lowered African topography, the conditions were not favorable enough to maintain a closed rainforest. A discussion of the results with respect to other model studies indicates a minor importance of vegetation-atmosphere or ocean-atmosphere feedbacks and a large dependence of the simulated vegetation response on the land surface/vegetation model.

Eurasian Neogene large herbivorous mammals and climate

The development and changes in the distribution of herbivorous mammal communities during the Neogene is complex. The Eurasian scale environmental patterns reflect the large scale geographical and climatic patterns. The reorganization of these affect the biome distribution throughout the continent. The distribution of mammal taxa was closely associated with the distribution of biomes. In Eurasia the Neogene development of environments was twofold. The early and middle Miocene that seemed to have been advantageous for mammals was followed by drying of environments during the late Neogene. The mid-latitude drying was the main trend, and it is the combined result of the retreat of Paratethys, the uplift of Tibetan Plateau and changes in the ocean currents and temperatures. The common mammals were "driving" the evolution of mammalian communities. During the late Miocene we see the drying affecting more and more regions, and we see changes in the composition of mammalian communities.

Analysis of large-amplitude stratospheric mountain wave event observed from the AIRS and MLS sounders over the western Himalayan region

Mountain waves in the stratosphere have been observed over elevated topographies using both nadir-looking and limb-viewing satellites. However, the characteristics of mountain waves generated over the Himalayan Mountain range and the adjacent Tibetan Plateau are relatively less explored. The present study reports on three-dimensional (3-D) properties of a mountain wave event that occurred over the western Himalayan region on 9 December 2008. Observations made by the Atmospheric Infrared Sounder on board the Aqua and Microwave Limb Sounder on board the Aura satellites are used to delineate the wave properties. The observed wave properties such as horizontal (lambda(x), lambda(y)) and vertical (lambda(z)) wavelengths are 276 km (zonal), 289 km (meridional), and 25 km, respectively. A good agreement is found between the observed and modeled/analyzed vertical wavelength for a stationary gravity wave determined using the Modern Era Retrospective Analysis for Research and Applications (MERRA) reanalysis winds. The analysis of both the National Centers for Environmental Prediction/National Center for Atmospheric Research reanalysis and MERRA winds shows that the waves are primarily forced by strong flow across the topography. Using the 3-D properties of waves and the corrected temperature amplitudes, we estimated wave momentum fluxes of the order of similar to 0.05 Pa, which is in agreement with large-amplitude mountain wave events reported elsewhere. In this regard, the present study is considered to be very much informative to the gravity wave drag schemes employed in current general circulation models for this region.

Analysis of large-amplitude stratospheric mountain wave event observed from the AIRS and MLS sounders over the western Himalayan region

Mountain waves in the stratosphere have been observed over elevated topographies using both nadir-looking and limb-viewing satellites. However, the characteristics of mountain waves generated over the Himalayan Mountain range and the adjacent Tibetan Plateau are relatively less explored. The present study reports on three-dimensional (3-D) properties of a mountain wave event that occurred over the western Himalayan region on 9 December 2008. Observations made by the Atmospheric Infrared Sounder on board the Aqua and Microwave Limb Sounder on board the Aura satellites are used to delineate the wave properties. The observed wave properties such as horizontal (lambda(x), lambda(y)) and vertical (lambda(z)) wavelengths are 276 km (zonal), 289 km (meridional), and 25 km, respectively. A good agreement is found between the observed and modeled/analyzed vertical wavelength for a stationary gravity wave determined using the Modern Era Retrospective Analysis for Research and Applications (MERRA) reanalysis winds. The analysis of both the National Centers for Environmental Prediction/National Center for Atmospheric Research reanalysis and MERRA winds shows that the waves are primarily forced by strong flow across the topography. Using the 3-D properties of waves and the corrected temperature amplitudes, we estimated wave momentum fluxes of the order of similar to 0.05 Pa, which is in agreement with large-amplitude mountain wave events reported elsewhere. In this regard, the present study is considered to be very much informative to the gravity wave drag schemes employed in current general circulation models for this region.

The impact of latent heating on the location and strength of the tropical easterly jet

The tropical easterly jet (TEJ) is a prominent atmospheric circulation feature observed during the Asian summer monsoon. It is generally assumed that sensible heating over the Tibetan Plateau directly influences the location of the TEJ. However, other studies have suggested the importance of latent heating in determining the jet location. In this paper, the relative importance of latent heating on the maintenance of the TEJ is explored through simulations with a general circulation model. The simulation of the TEJ by the Community Atmosphere Model, version 3.1 is discussed in detail. These simulations showed that the location of the TEJ is well correlated with the location of the precipitation. Significant zonal shifts in the location of the precipitation resulted in similar shifts in the zonal location of the TEJ. These zonal shifts had minimal effect on the large-scale structure of the jet. Further, provided that precipitation patterns were relatively unchanged, orography did not directly impact the location of the TEJ. These changes were robust even with changes in the cumulus parameterization. This suggests the potential important role of latent heating in determining the location and structure of the TEJ. These results were used to explain the significant differences in the zonal location of the TEJ in the years 1988 and 2002. To understand the contribution of the latitudinal location of latent heating on the strength of the TEJ, aqua-planet simulations were carried out. It has been shown that for similar amounts of net latent heating, the jet is stronger when heating is in the higher tropical latitudes. This may partly explain the reason for the jet to be very strong during the JJA monsoon season.

Dynamics of the East Asian Summer Monsoon in Present and Future Climates

This thesis aims at enhancing our fundamental understanding of the East Asian summer monsoon (EASM), and mechanisms implicated in its climatology in present-day and warmer climates. We focus on the most prominent feature of the EASM, i.e., the so-called Meiyu-Baiu (MB), which is characterized by a well-defined, southwest to northeast elongated quasi-stationary rainfall band, spanning from eastern China to Japan and into the northwestern Pacific Ocean in June and July.

We begin with an observational study of the energetics of the MB front in present-day climate. Analyses of the moist static energy (MSE) budget of the MB front indicate that horizontal advection of moist enthalpy, primarily of dry enthalpy, sustains the front in a region of otherwise negative net energy input into the atmospheric column. A decomposition of the horizontal dry enthalpy advection into mean, transient, and stationary eddy fluxes identifies the longitudinal thermal gradient due to zonal asymmetries and the meridional stationary eddy velocity as the most influential factors determining the pattern of horizontal moist enthalpy advection. Numerical simulations in which the Tibetan Plateau (TP) is either retained or removed show that the TP influences the stationary enthalpy flux, and hence the MB front, primarily by changing the meridional stationary eddy velocity, with reinforced southerly wind on the northwestern flank of the north Pacific subtropical high (NPSH) over the MB region and northerly wind to its north. Changes in the longitudinal thermal gradient are mainly confined to the near downstream of the TP, with the resulting changes in zonal warm air advection having a lesser impact on the rainfall in the extended MB region.

Similar mechanisms are shown to be implicated in present climate simulations in the Couple Model Intercomparison Project - Phase 5 (CMIP5) models. We find that the spatial distribution of the EASM precipitation simulated by different models is highly correlated with the meridional stationary eddy velocity. The correlation becomes more robust when energy fluxes into the atmospheric column are considered, consistent with the observational analyses. The spread in the area-averaged rainfall amount can be partially explained by the spread in the simulated globally-averaged precipitation, with the rest primarily due to the lower-level meridional wind convergence. Clear relationships between precipitation and zonal and meridional eddy velocities are observed.

Finally, the response of the EASM to greenhouse gas forcing is investigated at different time scales in CMIP5 model simulations. The reduction of radiative cooling and the increase in continental surface temperature occur much more rapidly than changes in sea surface temperatures (SSTs). Without changes in SSTs, the rainfall in the monsoon region decreases (increases) over ocean (land) in most models. On longer time scales, as SSTs increase, rainfall changes are opposite. The total response to atmospheric CO^2 forcing and subsequent SST warming is a large (modest) increase in rainfall over ocean (land) in the EASM region. Dynamic changes, in spite of significant contributions from the thermodynamic component, play an important role in setting up the spatial pattern of precipitation changes. Rainfall anomalies over East China are a direct consequence of local land-sea contrast, while changes in the larger-scale oceanic rainfall band are closely associated with the displacement of the larger-scale NPSH. Numerical simulations show that topography and SST patterns play an important role in rainfall changes in the EASM region.

Paleoenvironmental records from the Quelccaya ice cap, Peru and preliminary results from the Dunde ice cap, China [abstract]

EXTRACT (SEE PDF FOR FULL ABSTRACT): The 1000 year records of particulate deposition (soluble and insoluble), oxygen isotopic ratios, and net accumulation from the Quelccaya ice cap are presented. The net accumulation record from Quelccaya is shown to serve as a reasonable proxy for the water levels in Lake Titicaca. ... The ice core record from the Dunde ice cap offers the potential to reconstruct a very detailed history of environmental conditions on the Tibetan Plateau for the last 3000 years.

高山松的二倍体杂种起源-来自三个基因组的证据

利用松科植物特殊的遗传体系（叶绿体基因组一父系遗传、线粒体基因组—母系遗传、核基因组一双亲遗传），我们对高山松及其两个亲本种进行了广泛的群体取样，通过线粒体基因nadl、叶绿体基因rbcL和trnL-F基因间区以及低拷贝核基因4CL的序列分析或PCR-RFLP分析，为高山松同倍体杂种起源假说提供了翔实的遗传学证据，同时在个体水平上探讨了高山松不同群体的遗传组成、群体遗传结构、基因交流方向、群体建立过程以及杂种基因组的进化。具体结果如下： 1．细胞质基因组分析 1)线粒体基因nudl分析 本研究对油松、高山松和云南松的19个群体、295个个体的线粒体基因nadl的一个内含子进行了序列分析或PCR-RFLP分析，共检测到3种线粒体DNA单倍型-A、B和C。油松所有的取样群体仅含单倍型A;除BX群体外，所有的云南松群体仅含单倍型B; 10个高山松群体中，5个群体固定单倍型A，4个群体固定单倍型B，1个群体(ZD)分布有A和B两种单倍型。2)叶绿体rbcL基因分析 对同一组群体的rbcL基因进行序列分析或PCR-RFLP分析，共检测到两个变异位点和三种叶绿体单倍型（TT、TC和GC）。TT和GC分别是油松和云南松种特异性叶绿体单倍型，而在高山松群体里则三种单倍型均有分布，而且TC单倍型广泛地分布在7个杂种群体中，该单倍型很可能来源于点突变或第三个已灭绝的亲本。rbcL基因检测到的高山松群体分化系数很高(Gst=0.533)。 3)叶绿体trn L-F区序列分析 叶绿体trnL-F分子标记检测到的不同单倍型的差异主要是由引物“e”下游120碱基处一个多聚T结构的长度变异所致（叶绿体SSR位点）。10个高山松群体中共检测到5种叶绿体单倍型，其中两种主要的单倍型(9T和11T)分别为油松和云南松的种特异性单倍型，其他单倍型均为非典型单倍型。群体遗传结构分析表明：杂种群体表现最高的遗传多样性，而且trnL-F分析得到的高山松群体的分化系数也很高( Gst=0.443)。 总之，对高山松、油松和云南松的同一组群体取样进行的细胞质基因组分析表明：高山松群体分布有油松和云南松种特异性的线粒体和叶绿体单倍型，该细胞质DNA单倍型的地理分布为假说“高山松为油松和云南松的的二倍体杂种”提供了翔实的遗传学证据。油松和云南松在不同的杂种群体中分别做父本和母本，即两亲本在杂交过程中发生了双向基因交流。群体遗传结构分析发现高山松群体表现最高的遗传多样性，而且群体间的分化系数很高。不同的杂种群体在遗传组成上的差异表明他们经历过不同的建立和进化历史。从线粒体和叶绿体单倍型的地理分布可以看出杂种群体的建立曾经历强烈的奠基者效应和回交。青藏高原的隆升对高山松的起源、杂种群体的适应辐射以及保持产生了重要的影响。川西南和滇西北作为青藏高原的东边边界，很可能是当初云南松和油松分布的重叠区及杂交地带，即高山松的起源地。 2．核基因4CL分析 对高山松、油松和云南松的19个群体、32个个体的低拷贝核基因4CL进行了克隆及序列分析，获得的78条序列可分为两种类型（类型A和类型B）。这两种类型明显的差别是类型A相对于类型B在内含子区有- 20bp的缺失。以华山松的3条序列为外类群，对得到的78条序列进行基因谱系分析，发现所有的序列分成明显的两支，分别对应于类型A和类型B，而且每一支均包含三个种的部分序列，表明4CL基因在这三个种分化之前就已发生重复。另一个明显的特点是某个种的一条序列与另一个种的序列比其与同种的其他序列关系更近，可能因基因交流（杂交和渐渗）、非共祖、致同进化和重组等进化事件所致。三种松树中共检测到4CL基因序列的两种类型和六个亚类型，高山松群体中没有发现杂种独特的类型或亚类型。高山松和云南松共享三种序列亚类型以及最多的序列多态性，表明这两个种之间曾存在广泛的基因交流。

长花马先蒿的居群遗传变异与生物地理学

青藏高原地区是我国植物物种多样性和特有性最高的地区，且作为东亚植物区系的一个现代分化中心受世人瞩目。长花马先蒿是青藏高原高山草甸的广布种，其地理分布格局的形成与高原的隆升和气候变迁有着密切关系。因此，对长花马先蒿进行谱系生物地理学研究，有助于探讨青藏高原地区物种快速分化的机制和群体建立过程。 本研究对长花马先蒿11个居群、188个个体的叶绿体DNA trnT-trnF区进行了序列分析，发现该片段的长度变异范围为1441-1472bp。对位排列后的矩阵（含外类群）长1534bp，内类群中含33个碱基替换和 17 个插入/缺失,可分为20种单倍型。11个地理居群的总核苷酸多态性（π）为0.00468，单倍型多态性（Hd）为0.853，居群间的遗传变异（FST）高达88.2％，说明长花马先蒿具有很高的遗传多样性，且居群间发生了强烈遗传分化。 系统发育和遗传多样性分析发现长花马先蒿的20种叶绿体单倍型可归于四个地理单元——川西高海拔地区、川北地区、云南德钦地区及川藏地区。进一步分析发现：4个地理单元间存在着显著的遗传分化, 说明长花马先蒿具有明显的谱系地理分布格局。其中川西高海拔地区的四种主导单倍型构成了系统发育树最基部的一支，而以川西地区为中心、向南扩展至云南的两个居群所包含的几种单倍型均属于比较进化的类型。单倍型的网络关系(Network) 显示出西藏、青海、云南及四川北部的一些单倍型间遗传差异很小，亲缘关系很近。上述结果表明：长花马先蒿群体在冰期后的重新扩张过程主要表现为由南往北的递进式扩散，第四纪冰期气候的反复波动导致了该物种居群随生境变化而不断扩张或收缩,形成了现今的分布格局。初步推测川西地区很可能曾是长花马先蒿在第四纪冰期时的重要避难所，瓶颈效应和奠基者效应对其遗传多样性分布格局有重要影响。