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81.
The phase of semi-diurnal tides (M2 and S2) propagates clockwise in the central part of the Gulf of Thailand, although that of the diurnal tides (K1, O1 and P1) is counterclock-wise. The mechanism of clockwise phase propagation of semi-diurnal tides at the Gulf of Thailand in the
northern hemisphere is examined using a simple numerical model. The natural oscillation period of the whole Gulf of Thailand
is near the semi-diurnal period and the direction of its phase propagation is clockwise, mainly due to the propagation direction
of the large amplitude part of the incoming semi-diurnal tidal wave from the South China Sea. A simplified basin model with
bottom slope and Coriolis force well reproduces the co-tidal and co-range charts of M2 tide in the Gulf of Thailand. 相似文献
82.
83.
Participatory and Integrated Research in Mountainous Regions of Thailand and Vietnam: Approaches and Lessons Learned 总被引:1,自引:1,他引:0
Andreas Neef Franz Heidhues Karl Stahr Pittaya Sruamsiri 《山地科学学报》2006,3(4):305-324
Introduction Until the late 1980s, the mountainous regions of northern Thailand and northern Vietnam were largely cut off from the rapid economic develop- ment in the urban centers such as Bangkok, Chiang Mai and Hanoi, and from the dynamics of the ‘gree… 相似文献
84.
A brief summary of Dr. G. V. Rao's research interests is presented. Many of his earlier studies were in conjunction with the
summer Monsoon Experiment of 1979 (MONEX-79). These included: 1) the structure of the Somali jet based on aerial observations;
2) sea-level air trajectories over the equatorial Indian Ocean; 3) structural features of the east African low-level flow;
4) effects of Indian Ocean surface temperature anomaly patterns on the summer monsoon circulations; 5) structures of the monsoon
low-level flow over the Arabian Sea; 6) characteristics and momentum-flux budgets of the Arabian Sea convective bands; and
7) evaporation and precipitation over the Arabian Sea during the monsoon seasons. Dr. Rao's research efforts in recent years
had focused on case studies of mesocyclones spawned by tropical cyclones (TCs) in Florida using Doppler radar data and a mesoscale
numerical model. These included: 1) research on tornadic mesocyclones spawned by TC Earl in 1998; 2) documentation of subtle
differences between tornadic and non-tornadic mesocyclones in TC Floyd in 1999; and 3) numerical simulation of the tornadic
environment observed in peninsular Florida during TC Earl in 1998. Preliminary findings show that the supercells' cold pools
interacted with an existing boundary resulting in increased baroclinicity and horizontal vorticity, and a maximization of
the tornado production potential by the updrafts. The model successfully simulated the mesoscale features of the mesocyclones
and the tornadic environment observed during TC Earl. A 24 h simulation of accumulated rainfall within the inner domain agreed
well with the observed precipitation pattern over the region. 相似文献
85.
In a confined alluvial aquifer located between two rivers, discrete zones of anomalously high concentrations of redox species such as iron, are thought to be a result of groundwater flow dynamics rather than a chemical evolution along continuous flow paths. This new hypothesis was confirmed at a study site located between Nan and Yom rivers in Phitsanulok, Thailand, by analyzing concentrations of redox species in comparison with dynamic groundwater flow patterns. River incision into the confined alluvial aquifer and seasonally varying river stages result in truncated flow paths. The groundwater flow dynamics between two rivers has four phases that are cyclic, including: aquifer discharge into both rivers, direct flow from one river toward another, aquifer recharge from both rivers, and reverse of river-to-river flow. The resulting groundwater flow direction has a zigzag pattern and its general trend is almost parallel to the river flow. High iron anomaly appears as discrete zones in the transition areas of the confined alluvial aquifer because the lateral recharge from rivers penetrates into the aquifer only by tens of meters. The high iron anomaly, which is nearly constant in space and time, is a result of groundwater/surface-water interactions and related groundwater flow dynamics. 相似文献
86.
The tsunami of 2004 in the Indian Ocean transported thousands of meters-long boulders shoreward at Pakarang Cape, Thailand. We investigated size, position and long axis orientation of 467 boulders at the cape. Most of boulders found at the cape are well rounded, ellipsoid in shape, without sharp broken edges. They were fragments of reef rocks and their sizes were estimated to be < 14m3 (22.7t). The distribution pattern and orientation of long axis of boulders reflect the inundation pattern and behavior of the tsunami waves. It was found that there is no clear evidence indicating monotonous fine/coarse shoreward trends of these boulders along each transect line. On the other hand, the large boulders were deposited repeatedly along the three arcuate lines at the intertidal zone with a spacing of approximately 136m interval. This distribution pattern may suggest that long-lasting oscillatory flows might have repositioned the boulders and separated the big ones from small. No boulders were found on land, indicating that the hydraulic force of the tsunami wave rapidly dissipated on reaching the land due to the higher bottom friction and the presence of a steep slope. We further conducted numerical calculation of tsunami inundation at Pakarang Cape. According to the calculation, the sea receded and the major part of the tidal bench (area with boulders at present) was exposed above the sea surface before the arrival of the first tsunami wave. The first tsunami wave arrived at the cape from west to east at approximately 130min after the tsunami generation, and then inundated inlands. Our calculation shows that tsunami wave was focused around the offshore by a small cove at the reef edge and spread afterwards in a fan-like shape on the tidal bench. The critical wave velocities necessary to move the largest and average-size boulders by sliding can be estimated to be approximately 3.2 and 2.0m/s, respectively. The numerical result indicates that the maximum current velocity of the first tsunami wave was estimated to be from 8 to 15m/s between the reef edge and approximately 500m further offshore. This range is large enough for moving even the largest boulder shoreward. These suggest that the tsunami waves that were directed eastward, struck the reef rocks and coral colonies, originally located on the shallow sea bottom near the reef edge, and detached and transported the boulders shoreward. 相似文献
87.
This article sketches the process of democratization in Thailand, focusing on shifting relations between civil society and state actors. Environmental discourse and conflicts about natural resources, specifically forests, during the last two decades, have been one of the main fields of social controversy and change. In the context of these controversies, civil society actors, in resistance to and alliance with state agencies, drove forward democratization by intruding into power domains of the state. State agents, increasingly forced to justify their actions according to democratic norms in the expanding space of public debate, had to search for allies and majorities within civil society. The successful establishment of public debate as an integral part of political decision making, on the one hand, resulted in a diversification of civil society, on the other hand, forced powerful segments of society to organize and defend their interests within the new public political space. Strategies of exclusion, referring to nationalism and ethnicism, have become an important instrument to secure positions and power, threatened in the process of democratization and emancipation of discriminated social groups. 相似文献
88.
89.
中国海和泰国湾海域海平面的经向涛动 总被引:1,自引:0,他引:1
卫星高度计遥感海面高度距平资料(1992-2012年)的分析结果证实中国海(渤、黄、东海及南海)和泰国湾作为一个半封闭的狭长水域,其海平面存在显著的南北经向涛动。涛动呈现明显的季节性,冬季南高北低,夏季北高南低,以渤海和泰国湾的海平面高差作为涛动的测度,其多年平均波动幅度达63cm,较差超过80cm。时间序列分析显示,在季节尺度上这一涛动几乎完全受东亚季风的支配,表明东亚季风的局地强迫是造成季节涛动的主要原因。进一步的分析发现,除季节波动之外研究海域海平面的经向涛动还存在明显的年际变化。不过,与季节尺度的波动有所不同,经向涛动的年际变化不仅是东亚季风区局地作用的结果,而且与太平洋海盆尺度的大气强迫有关,其作用与季风在同一数量级。涛动的年际变化大致滞后各气候因子两个月。采用多输入线性模型做偏相关分析筛选的结果显示,除东亚季风指数之外,研究海域的海平面涛动指数主要与太平洋的南方涛动指数(SOI)和西太平洋遥相关指数(WP)相关。这表明外部强迫既来自热带,也来自中纬度。南方涛动所导致的赤道海域海平面的东西向年际涛动,以及中纬度西风急流年际波动对西北太平洋海平面的作用,都有可能导致研究海域海平面经向涛动的年际变化,其机制有待进一步探讨。 相似文献
90.
Geochemical analysis reveals that Middle Triassic radiolarian cherts from northern Thailand,including Chiang Dao,Lamphun and Den Chai,are of biogenic origin.These cherts present slightly high SiO2 content which was possibly modified by diagenetic alteration and migration processes as indicated by negative correlation between SiO2 and most of the other major elements.The relatively high content of Cr,Zr,Hf,Rb and Th and high positive correlation of these elements with Al and Ti from the majority of cherts su... 相似文献