气候学 地方气候、小气候与应用气候

P4022007010036中国第二次北极科学考察路线上温室气体瓶采样结果分析=A result of greenhouse gases flask-sampled on the course of the 2nd Chinese Arctic research expedition,2003/张东启,徐建中…∥冰川冻土.—2006,28(3).—319~323研究结果表明:海洋表面不同纬度带上C     

地方气候、小气候与应用气候

P467 2007021016长江源沱沱河区45a来的气候变化特征=Climate change in Tuotuohe area at the headwaters of Yangtze River/张国胜,时兴合…//冰川冻土．—2006,28(5)．—678～685利用1959-2003年长江源区沱沱河气象站气温、降水、积雪等地面观测资料,对年代际的气候变化特征及其影响进行了分析．结果表明:该区域45a来夏季增温比较明显．     

地方气候、小气候与应用气候

S792.112006010041毛乌素沙地杨树年轮结构对气候因子的响应=Response oftree-ring structure of poplar to cli mate factors in the Mu UsDesert/黄荣凤,古川郁夫…∥北京林业大学学报.—2005,27(3).—24~29图3表2参16(姚则安)BeP463.222006010042中国东北森林气象因子与NDVI     

生态学

P9012006010762干旱区绿洲景观尺度稳定性初步分析=Preli minary analysison the oasis stability at the landscape level in the arid regions/罗格平,周成虎…∥干旱区地理.—2004,27(4).—471~476在景观尺度上,从绿洲景观多样性、景观廊道的复杂性以及土地利用及其生态环境     

地方气候、小气候与应用气候

P426.616.P456.82003031 961金华旱涝趋势统计分析=Statisrieal anal邓i、of drought一floodrrend in Jinhua/冯利华//长江流域资源与环境一2003,12(2)一169一173图2表5参3(宋金叶)HNP422.4 2003031962青藏高原西部的地面热源强度及地面热且平衡=The inter-sity of surfaee heat souree and surfaee heat balanee on the west-ern Qinghai一Xizang plareau李国平,段廷扬…//地理科学一2003,23(l)一13一18 以1997至1998年青藏高原西部改则和狮泉河地区自动气象站连续观测的近地层梯度资料,采用廓线一通量法计算出观测期逐日的总体输送系…     

气候成因、要素与气候变化

P4672006010009兰州与江汉平原有机碳同位素的古气候指示意义对比研究=Paleocli matic i mplication of Lanzhou and Jianghan plain:acli mate proxy study of organic carbonisotope/杨桂芳,彭红霞…∥长江流域资源与环境.—2005,14(4).—486~490研究结果表明:在兰州地区,δ13Corg值波动反映C3/C4植物比例的改变,指标温度变化.δ13Corg值偏正时,表明C4植物含量较大,反映温度较高.而δ13Corg值偏负时,表明气候较冷;汉江平原δ13Corg值主要反映降水信息,δ13Corg值偏负时指示相对暖湿气候,δ13Corg值偏正反映气候偏干.δ13Corg等指标…     

新疆气候时空变化特征及其趋势(英文)

Temperature and precipitation time series datasets from 1961 to 2005 at 65 meteorological stations were used to reveal the spatial and temporal trends of climate change in Xinjiang, China. Annual and seasonal mean air temperature and total precipitation were analyzed using Mann-Kendall (MK) test, inverse distance weighted (IDW) interpolation, and R/S methods. The results indicate that: (1) both temperature and precipitation increased in the past 45 years, but the increase in temperature is more obvious than that of precipitation; (2) for temperature increase, the higher the latitude and the higher the elevation the faster the increase, though the latitude has greater influence on the increase. Northern Xinjiang shows a faster warming than southern Xinjiang, especially in summer; (3) increase of precipitation occurs mainly in winter in northern Xinjiang and in summer in southern Xinjiang. Ili, which has the most precipitation in Xinjiang, shows a weak increase of precipitation; (4) although both temperature and precipitation increased in general, the increase is different inside Xinjiang; (5) Hurst index (H) analysis indicates that climate change will continue the current trends.     

气候学

气候成因、要素与气候变化P642.142006032025青藏高原地气温度之间的关系=The relationship between airtemperature and ground temperaturein the Tibetan Plateau/李述训,吴通华∥冰川冻土.—2005,27(5).—627~632图4表3参7(洪明)BiP461.62006032026乌鲁木齐河源区44a来气候     

地貌学

P512.22006021122长江口九段沙现代潮滩沉积特征=Sedi mentary characteris-tics of the modern tidal flat of Jiuduansha shoal in Changjiangestuary/谢小平,王兆印…∥沉积学报.—2005,23(4).—566~573根据2003年对长江河口九段沙潮间带和潮上带的现场调查和室内对沉积构造     

陆地地貌

P512.22007010146江苏中部淤泥质潮滩潮汐层理成因机理和风暴沉积判别标志=Mechanism of silt-mud couplet of mud tidal flat and discrimination criteria of storm surge sedimentation in the middle Jiangsu province/王建,柏春广…∥沉积学报.—2006,24(4).—562~569通过     

海洋水文

P7312006010080粤西水东单点系泊海域潮流和低频流特征=The character-istics of low frequency currents in the area of Shuidong an-chored floating whelf in the west of Guangdong coastal waters/严金辉,陈达森∥海洋湖沼通报.—2005(3).—8~15图4表2参6(许桂红)NX8242006010081长江口及其邻近海域悬浮物浓度和浊度的对应关系=Cor-responding relationship betweensuspended matter concentrationand turbidity on Changjiang estuary and adjacent sea area/翟世奎,张怀静…∥环境科学学报.—2005,25(5).—693~699根据该次调查…     

气候成因、要素与气候变化

P4672007042850西北地区45a来降水异常的时空变化及其标度特征=Spa-tial and temporal variations and scaling of precipitation overNorthwestChina during1960-2004/苏布达,王国杰…∥冰川冻土.—2007,29(2).—176~182研究表明:西北地区降水自东南向西北逐步递减,降水变化趋     

地方气候、小气候与应用气候

P468 20伽闭31807长江三峡水库气候效应数值模拟二N~司m团elingof而~llmate eftectsp找妇uc侧」by the formation of tha Three励rgesReservoirregon/张洪涛,祝昌汉…//长江流域资源与环境一2004,13(2)一133一137图7表3参6(宋金叶) HNP333。12以冲旧1808中国东北地区地表水资源与气候变化关系的研究二Rda-tlo们‘hiP between elimate vanation and su州触ee water~inNorth“达tChina/孙力,安刚…//地理科学一20(抖,24(1)一42一49 东北地区地表水资源各分量与气温和降水之间有春较 .7。好的相关哭系.健建立了气盆和灯成梦降水变化对水资…     

气候成因、要素与气候变化

P467 2003042865中国西北现代气候变化事实与未来趋势展望二Tl*Pr璐entfaets and the future tendeney of the elimate ehange in North-west Chilla/李栋梁,魏丽…//冰川冻土一2003,25(2)一135一142 利用西北地区建站至2000年常规气象观测站资料及美国NCEP/NCAR再分析全球网格点资料,分析了西北地区现代气候变化的特点,揭示了西北地区气候由暖干转向暖湿的事实,在此基础上对未来几十年气候变化趋势作了估计.图7参14(洪明)BiP426.614 200304286620世纪西北地区降水且变化特征=Changing feature。of pre-eiPitation over Northwest C…     

气候学 气候成因、要素与气候变化

P4342007010004新疆夏季变湿的大气环流异常特征=Atmospheric circulation anomalies during wetting summer over Xinjiang region/赵兵科,蔡承侠…∥冰川冻土.—2006,28(3).—434~442研究结果表明:在平均环流场上,中亚-巴尔喀什湖槽及上下游地区脊的增强是新疆地区夏季变湿的     

社会、经济地理

F1272006010309南水北调中线工程与汉江中下游地区可持续发展=Effectof the middle route Project of South to North Water Transferon the sustainable development of the middle andlower reachesof Hanjiang River/蔡述明,殷鸿福…∥长江流域资源与环境.—2005,14(4).—40     

气候成因、要素与气候变化

P732 2007020977冬季北大西洋海温年际、年代际变化与中国气温的关系= Relation between interannual,interdecadal variability of SST in North Atlantic in winter and air temperature in China/曲金华,江志红…//地理科学．—2006,26(5)．—557～563利用NCEP/NCAR月平均再分析资料海洋表面月平均温度资料、500hPa月平均高度场以及中国160站月平均气     

湖沼学

P333.12007042944天目湖水文特征变化及其对上游湿地和湖泊生态环境的影响=Variation of hydrological characteristics of Tianmu Lakeandits effect on the Tianmuhu wetland and ecological environ-ment of the Tianmu Lake/黄群芳,张运林…∥湿地科学.—2007,5(1).—51~57     

地方气候、小气候与应用气候

P468 .P463.21 2004010047河北省怀来盆地近30年的气候变化与起沙扬尘间的关系=Relatlonship between elimate ehanges over 30 years alld sandst〔”刀latHuailaibasin/娄安如//北京师范大学学报.自然科学版一2003,39(4)一531一536 通过对河北省怀来盆地1970一1999年的气象数据分析,认为怀来盆地近30a的气候变化规律是:年平均气温在逐年上升,年降水量在逐年下降,地面年水分蒸发量略有下降,大风天气明显减少,但大风天气的出现却很集中,分析了这样的气候条件与大面积裸露的沙化土地是导致怀来盆地起沙扬尘的主要原因,同时提出了起沙扬尘的…     

塔克拉玛干沙漠沙尘演变及气候因素分析

Based on the sand dust storms data and climatic data in 12 meteorological stations around sand dust storm originating areas of the Taklimakan Desert, we analyzed the trends of the number of dust storm days from 1960 to 2005 as well as their correlations with temperature, precipitation, wind speed and the number of days with mean wind speed 〉 5 m/s. The results show that the frequency of dust storm events in the Taklimakan region decreased with the elapse of time. Except Ruoqiang and Minfeng, in the other 10 meteorological stations, the frequency of dust storm events reduces, and in 4 meteorological stations of Kuqa, Korla, Kalpin and Hotan, the frequency of dust storm events distinctly decreases. The temperature has an increasing trend, while the average wind speed and the number of days with mean wind speed ≥ 5 m/s have decreasing trends. The correlation analysis between the number of days of dust storms and climatic parameters demonstrates that wind speed and the number of days with mean wind speed 〉 5 m/s have strong positive correlation with the number of days of dust storms, with the correlations coefficients being 0.743 and 0.720 （p〈0.01）, respectively, which indicates that strong wind is the direct factor resulting in sand dust storms. Whereas precipitation has significant negative correlation with the number of days of dust storms （p〈0.01）, and the prior annual precipitation has also negative correlation, which indicates that the prior precipitation restrains the occurrence of sand dust storms, but this restraining action is weaker than the same year＇s precipitation. Temperature has negative correlation with the number of dust storm days, with a correlations coefficient of -0.433 （p〈0.01）, which means that temperature change also has impacts on the occurrence of dust storm events in the Taklimakan region.