气候

The weather of this year is a lot hotter than that of last year.

今年的气候比上一年的气候要热得多。

And human activities play an important role in the process of hydrological changes, especially in hydro chemical changes.

水文特征主要是由一定的区域地形和气候条件决定的，就短时间尺度而言，气候和人为因素影响更为明显。

Under the hypothetic climate change scenarios of 20% change in precipitation and –2℃ change in temperature, annual runoff in the four regions will increase 37.8%, 62.3%, 73.2% and 48.2% respectively in order.

根据黄河上中游未来气候的可能变化，假定的气候变化方案为：降水变化为±20%、±10%和不变，同时气温保持不变及变化±1℃、±2℃共25种组合。

An Indian summer" is when it is 10 hot and sunny later in the year then usual.

"印度夏天"指的是岁末时，如果 10 气候比常年热阳光照射比较强烈的气候。

Due to the nonlinear property of climate system, climate change responds nonlinearly to the insolation.

由于气候系统所具有的非线性性质，决定了气候变化对太阳辐射量变化的非线性响应。

Since PMIP (Paleoclimate Modeling Intercomparison Project) launched in 1994, it has got many fruits. Chinese scientists also have done quite a few researches in paleoclimate modeling.

国际古气候对比项目（PMIP，Paleoclimate Modeling Intercomparison Project）开展十多年来，取得了许多成果，我国科学家在古气候模拟方面也做了相当的研究。

Moreover, based on the boundary conditions recommended by the Paleoclimate Modelling Intercomparison Project, it is further indicated that vegetation feedback in East Asia, possible ice sheet over the Tibetan Plateau, and sea surface temperature reconstruction in the western Pacific different from the PMIP data source can induce additional climate effects, which partly reconcile model-paleodata discrepancies as displayed by the standard PMIP simulations.

在国际古气候模拟比较计划标准试验的基础上，进一步指出东亚植被的反馈作用、青藏高原可能冰川的反馈作用、以及西太平洋表面温度的作用能够引起额外的气候效应，可在一定程度上改进PMIP标准试验的模拟效果。

CMIP, the Coupled Model Intercomparison Project, established under the auspices of World Climate Research Program includes a series of intercomparison projects for global coupled oceanatmosphere general circulation models.

由世界气候研究计划推动制定的CMIP计划，是一整套耦合大气环流气候模式的比较计划。

We can distinguish two types of global climates which occurred intermittently in the past.

我们可以把全球性的气候分成两种类型，过去这两种气候轮替出现。

A comparative study of pollen floras between two cores: Core 17940 from the northern slope of the South China Sea and a core from the Toushe Basin in central Taiwan Province, reveals that there were three different vegetation types around the two areas during 15-40kaBP. The first type is characterized with the subtropical evergreen broadleaved forest during MIS2 (20-15kaBP). The second is the Pinus/Alnus-dominated woody plant communitites, corresponding to an interstadial summer monsoon dominated warm and humid climate and higher sea/lake level. The third is the Artemisia/Poaceae-dominated herb communities, corresponding to a stadial winter monsoon dominated warm and dry climate and lower sea/lake level.

根据南海北部17940孔和台湾中部头社孔孢粉序列对比结果，首次提出了华南地区15-40kaBP期间的三个具代表性植物群：1以青栲类为主的亚热带常绿阔叶林为第1植物群，该植物群在MIS2阶段(20-15kaBP)，为南海北部周边地区和台湾中部头社盆地周围地带性植被；2以松属或桤木属为主的木本植物为第2植物群，对应于间冰阶，夏季风盛行，降水充沛，气候暖湿，高海面；3以蒿属或以禾草为主的草本植物为第3植物群，对应于冰阶，冬季风盛行，降水少，气候暖干，低海面。

On the other hand, the more important thing is because the urban housing is a kind of heterogeneity products.

另一方面，更重要的是由于城市住房是一种异质性产品。

Climate histogram is the fall that collects place measure calm value, cent serves as cross axle for a few equal interval, the area that the frequency that the value appears according to place is accumulated and becomes will be determined inside each interval, discharge the graph that rise with post, also be called histogram.

气候直方图是将所收集的降水量测定值，分为几个相等的区间作为横轴，并将各区间内所测定值依所出现的次数累积而成的面积，用柱子排起来的图形，也叫做柱状图。