The spatial-temporal distribution of NPP along NECT and its response to climatic change were also analyzed. Results showed that the change tendency of NPP spatial distribution in NECT is quite similar to that of precipitation and their spatial correlation coefficient is up to 0.84 (P.01). The inter-annual variation of NPP in NECT is mainly affected by the change of the aestival NPP every year, which accounts for 67.6% of the inter-annual increase in NPP and their spatial correlation coefficient is 0.95 (P.01). The NPP in NECT is mainly cumulated between May and September, which accounts for 89.8% of the annual NPP. The NPP in summer accounts for 65.9% of the annual NPP and is the lowest in winter. Recent climate changes have enhanced plant growth in NECT. The mean NPP increased 14.3% from 1980s to 1990s. The inter-annual linear trend of NPP is 4.6 gCm^(-2)a^(-1), and the relative trend is 1.17%, which owns mainly to the increasing temperature.
结果表明：(1)NECT样带植被NPP的空间变化趋势同降水量的空间变化十分相似，由东到西逐渐降低，二者在空间上的相关性达到了0.84 (P.01)，说明NECT样带的植被NPP在空间分布上主要受水分趋动：(2)NECT样带植被NPP的年际变化主要是由各年份夏季NPP的变化造成的，夏季对NECT样带植被NPP的年际增长贡献率最大(67.6%)，二者之间的相关性达到了0.95 (P.01)；(3)NECT样带的植被NPP积累期主要发生在5-9月份，这5个月的NPP占了全年NPP总量的89.8%，整个夏季（6-8月份）的NPP占了全年的65.9%，冬季（12-2月份）的NPP最低，基本为0；(4)近19年来的气候变化促进了NECT样带的植被生长，从1980年代到1990年代，NPP显著增加，年代际相对增长率为14.3%，平均年际绝对增长趋势为4.6 gCm^(-2)a^(-1)，相对增长趋势为1.17%，这主要是由温度升高引起的。
The spatial-temporal distribution of NPP along NECT and its response to climatic change were also analyzed. Results showed that the change tendency of NPP spatial distribution in NECT is quite similar to that of precipitation and their spatial correlation coefficient is up to 0.84 (P 0.01). The inter-annual variation of NPP in NECT is mainly affected by the change of the aestival NPP every year, which accounts for 67.6％ of the inter-annual increase in NPP and their spatial correlation coefficient is 0.95 (P 0.01). The NPP in NECT is mainly cumulated between May and September, which accounts for 89.8％ of the annual NPP. The NPP in summer accounts for 65.9％ of the annual NPP and is the lowest in winter. Recent climate changes have enhanced plant growth in NECT. The mean NPP increased 14.3％ from 1980s to 1990s. The inter-annual linear trend of NPP is 4.6 gC·m-2·a-1, and the relative trend is 1.17％, which owns mainly to the increasing temperature.
结果表明：(1)NECT样带植被NPP的空间变化趋势同降水量的空间变化十分相似，由东到西逐渐降低，二者在空间上的相关性达到了0.84(P《0.01)，说明NECT样带的植被NPP在空间分布上主要受水分趋动；(2)NECT样带植被NPP的年际变化主要是由各年份夏季NPP的变化造成的，夏季对NECT样带植被NPP的年际增长贡献率最大(67.6％)，二者之间的相关性达到了0.95(P《0.01)；(3)NECT样带的植被NPP积累期主要发生在5-9月份，这5个月的NPP占了全年NPP总量的89.8％，整个夏季(6-8月份)的NPP占了全年的65.9％，冬季(12-2月份)的NPP最低，基本为0；(4)近19年来的气候变化促进了NECT样带的植被生长，从1980年代到1990年代，NPP显著增加，年代际相对增长率为14.3％，平均年际绝对增长趋势为4.6 gCm-2(a-1，相对增长趋势为1.17％，这主要是由温度升高引起的。
The milk yield records of Holstein cows on the Bayi and Wuchang da iry farms from 1995 to 1999 in Wuhan were collected and adjusted to standard lac t ation length of 305 days. One year was divided into three seasons considering th e special climatic characteristics of Wuhan.
收集了武汉市牛奶公司八一奶牛场和武昌奶牛场的1995～1999年的产奶量数据，在进行305 d产奶量校正后，采用动物模型BLUP原理和相应的计算机软件对数据进行了统计分析。
The successive three-year wheat summer sowing test from 1999-2001 reveals that the climatic and ecological condition from August to the beginning of November in the west suburb, Jingzhou city in chinese Jianghan plain meets the meets of wheat soming.
1999～2001年连续三年小麦夏季繁殖试验表明，地处江汉平原的荆州城西郊，8月初至11月中旬的气候生态条件基本能满足半冬性偏春性小麦的生育需要。
3When an above-normal (below-normal) winter TFSE happens, less ASE usually be seen over most northern Eurasia in November last year, but more ASE can be seen only in some European regions in February current year, which indicates that European winter AFSE may play an important role for climatic effects of winter TFSE.(4)As expected, three East Asian planetary scale circulation systems found to associate with winter TFSE.
对冬季欧亚大陆北部新增雪盖面积异常原因的初步分析表明，冬季TFSE异常偏多是冬末雪盖面积异常偏大和秋末雪盖面积异常偏小的共同作用，整体看来，秋末雪盖面积的异常偏少应更重要，冬季TFSE与秋末TSE的相关高达-0.81，但在欧洲部分地区，其冬末、秋末的雪盖面积变化对冬季TFSE异常变化来说都很重要。
By comparison with previous studies, I investigated the 22-year changes in interspecific association of the climatic climax vegetation in Dinghushan, Guangdong, China.
种间联结是指不同物种在空间分布上的相互关联性，通常是由于群落生境的差异影响了物种的分布而引起的[1，2]。
Company said that this year, the Fujian Refining and Ethylene Project construction to withstand the rainy season, typhoons, and other climatic factors as well as the cause overloaded with a large number of domestic and foreign manufacturing equipment and materials, and other adverse effects on the delivery lag.
公司表示，今年以来，福建炼油乙烯项目工程建设经受了雨季、台风等气候因素以及国内外制造业超负荷致使大批设备材料滞后交付等不利影响。
The 250 mm isohyet is used as the climatic boundary line between arid and semiarid region and it shifts at a maximum distance of 110-130 km during the extreme dry and wet year.
干旱半干旱过渡带是生态环境变化的敏感和脆弱地带，气候的波动性和人口压力是生态脆弱的根本原因，干旱和半干旱区交界线在丰枯年份的空间摆动幅度最大达110-130km。
Because temperature and precipitation have strong correlation in China (the correlation coefficient is about 0.77), so the author uses two kind of methods, one is Pearson correlation, and the other is partial correlation. The findings are:(1)The partial correlation is the better method than Pearson correlation; (2)The year-average temperature is an important climatic factor on influencing the carbon storage of soil. The correlation differ greatly in three cases: temperature0 degree, 1020 degree.(3)The correlation of non-agricultural soil carbon storage with climate factors is better than agricultural soil's. This means that carbon storage in agricultural soil is less influenced by natural climate factors due to the human management.
在分析中考虑了温度与降水之间存在较强的正相关(相关系数为0.77)这一前提，分别以皮尔逊相关和偏相关方法进行了分析，主要得出以下结论：①由于温度与降水的较强相关性，采用皮尔逊相关分析会得出一些错误的或不易解释的结论，而较好的分析方法是偏相关分析；②对所有样本进行的偏相关分析表明，土壤碳储量与温度和降水的相关性明显好于皮尔逊相关，而且土壤碳储量与温度和降水的相关程度相似；③温度影响着土壤碳储量与温度、降水的相关性大小和显著性，在温度小于10℃、温度介于10～20℃、温度大于20℃这三种情况下，它们之间的相关性存在很大的差异；④不管样本处于什么温度范围内，非耕地土壤碳储量与温度和降水的相关性均好于耕地土壤碳储量与温度和降水的相关性，这表明耕地土壤碳储量受自然因素影响强度降低了。
However, because of geological and climatic conditions, the Qinghai-Tibet Highway is the only one road which is open year-round.
但是，由于地理和气候条件的制约，实际上只有一条青藏公路能做到常年畅通。
One year was divided into three seasons considering the special climatic characteristics of China.
在模型中考虑的效应包括牛场、年度、季节、胎次、个体的育种值等，其中季节根据我国的气候特点划分为3个阶段。
The climatic trend demonstrated by changes of the lakes in Xinjiang since recent year.
胡汝骥，马虹，樊自立，等。近期新疆湖泊变化所示的气候趋势
This article mainly used 1971~2000 year-climate material to carry on the detailed analysis to Liaoning Province agriculture climatic resource present situation, and has carried on the discontinuity examination.
本文主要利用1971～2000年气候资料对辽宁省农业气候资源的现状进行le详细的分析，并进行了突变性检测。
Triangle Hill warm and humid climatic conditions and abundance of fertile soil conditions of the formation of a rich vegetation, the distribution of garden plants is 496 Section 138 of more than 1100 kinds, constitute a rich aesthetic landscape of forest resources, showing a quarter of the alternating phase and sex change, all year round with the quarter for King, beautiful spring, Baicao Zheng-chun, Yamahana brilliant, scene of prosperity, Cui Zhu Qing-Song; summer season, breezy and pleasant weather, home this summer, this music extremely Ho; autumn, Yushu Qionghua, Hongtoushan here, visitors now, relaxed and happy; winter season, snow, Yushu Qionghua, this赏雪, increasingly the North.
三角山温暖湿润的气候条件和丰沃的土壤条件形成了丰富的植被，园内植物分布达138科496属1100多种，构成了森林景观丰富的美学资源，呈现出季相和色相的交替变化，一年四季景随季换，春光明媚，百草争春，山花烂漫，莺歌燕舞，松清竹翠；盛夏时节，凉风习习，气候宜人，居此避暑，此乐何极；秋高气爽，玉树琼花，于此红透，游人至此，心旷神怡；隆冬季节，银装素裹，玉树琼花，于此赏雪，胜似北国。
This area occupies the subtropics monsoon plateau peak climatic province the edge, in the piedmont is growing a lot of year spruce, the pine and cypress, the forest covering the entire field, ancient wooden towering.
这个 地区处在亚热带季风高原高峰气候区域的边缘，山麓中生长着千百年的云杉、松柏，成林蔽野，古木参天。
The year guarantees the jade to occupy the subtropics monsoon plateau peak climatic province the edge, in the piedmont grows is doing hundred year spruce, the pine and cypress, the forest covering the entire field, ancient wooden towering.
年保玉则处在亚热带季风高原高峰气候区域的边缘，山麓中生长着干百年的云杉、松柏，成林蔽野，古木参天。
Base on the surface mass accumulation data in year of 1987/88, both distribution and variability of annual mass balance on Mizuho Plateau have been discussed. The authors also studied how they were influenced by means of shortterm climatic and topographical variations.
根据1987/1988年度表面物质积累资料，对Mizuho（瑞穗）高原该年度物质平衡的分布规律及其变化进行了讨论，同时还对年内短期天气过程及地形变化对物质平衡的影响进行了分析。
According to the seasonal aridity index. Fujian climate has been divided into six climatic patterns in humidity: humid throughout the year, dry in summer-autumn winter, dry in autumn-winter, dry in summer-autumn, dry in summer, and dry in autumn.
最后用季干燥度将全省分成全年湿润、夏干、秋干、夏秋干、秋冬干和夏秋冬干六种气候类型。
Because of the warm climatic conditions, which suitable for vegetation to grow, mountains are covered by year-round dense vegetation; bring quiet, simple, inoffensive aesthetic sense.
桂林由于自然气候条件温暖，适宜植被生长，所以终年有茂密的植被覆盖山体，给人带来宁静、质朴、与世无争的审美感受。
The year's harvest of 2004 is considered an abundant year by analyzing the agricultural climatic condition including light, temperature and precipitation in growth period of grain and oil crops, growth situation of crops and occurrence of meteorological disaster.
通过对2004年夏收粮油作物、秋收粮食作物生长期间的光热水、农作物生长情况和气象灾害发生程度等农业气候条件的分析，得出2004年为偏丰年景。