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961.
962.
根据闽东海洋环境监测中心2004年-2006年阂东沿岸生态调查的资料,分析和研究了闽东沿岸浮游植物的生态特征.共鉴定出浮游植物的种类3个门39属共134种,其中硅藻门的种类占总种数的80%,为该调查海域主要门类.主要优势种是中肋骨条藻(Skeletonema costatum)、旋链角毛藻(Chaetoceros curvisetus)、尖刺拟菱形藻(Pseudo—nitzschia pungens)和丹麦细柱藻(Leptocylindrus danicus)等.浮游植物的丰度分布,呈现由调查海域东北侧向西南侧、由近岸向远岸减少的空间特征,夏季高、春季低的季节变化特点,并且有逐年减少的年际变化趋势.本调查海域浮游植物多样性指数较高,群落较稳定. 相似文献
963.
近年来长江河口北支水沙特性与河槽稳定性分析 总被引:3,自引:0,他引:3
根据崇头、青龙港、三条港和连兴港1950~2001年潮汐潮流观测资料和2005年6~7月的大、中、小潮及2007年5月5~10日沿北支河槽进行的两个连续潮周期水、沙、盐的现场观测数据并结合参考2005年的实测地形图.通过对长时间序列(1950~2001年)的分流比、年均流量、潮位、潮历时等数据的整理分析并与近期(1998~2005年)的水文特征值比较,发现随着北支分流量逐渐减少,河槽内强烈的潮波已成为影响北支河槽不稳定的主要因素;青龙港近年来(1998~2005年)平均高、低潮位出现增高,比多年(1950~2001年)平均高、低潮位分别高出15和17cm,是北支河床近年来持续性淤浅的体现;大潮期间北支河槽涨潮含沙量无论量值还是扩散强度均大于落潮,明显表现出河口涨潮槽具有的泥沙运动规律.自2001年以来除少数年份的小潮汛外,均表现出明显的涨潮优势,其中2002年3月大潮的潮量优势流仅为9.42%,显示出涨潮优势十分明显,说明北支河槽近几年来正朝着衰退的过程发展;2005年北支河槽-2、-4和-6 m等深线均呈喇叭状,闭合端指向上游,符合涨潮槽的几何形态;再从河槽类型系数(λ)看,大潮期间λ值均大于1,最大值为31.1,涨潮槽特征显著;而洪季中、小潮各测站λ值均小于1,最小值为0.000 3,A、B两测站在大潮时λ值均大于1,而小潮时又都小于1,显示北支河槽虽主要表现为涨潮槽的特征,但洪季受径流和潮汛影响,其涨潮槽特性不稳定.总体而言,目前北支河槽为一条不稳定的废弃型涨潮槽. 相似文献
964.
根据板东构造板东4井等长兴组钻探资料,对长兴组的生物礁进行了研究。研究表明板东构造长兴组储集岩有生物(屑)泥晶灰岩-含生物(屑)泥晶灰岩、礁灰岩和白云岩。综合储集岩物性特征、区域钻、测井资料及野外剖面,总结了生物礁的形成与演化模式及模式各部位所对应的岩性和物性。通过地震响应特征、反演等技术建立了长兴组储层识别模式,利用对应速度、Landmark属性提取的储层有效厚度经计算机网格化编制出了长兴组储层厚度分布预测图,与钻测井厚度对比,证实板东4井生物礁为点礁。 相似文献
965.
Using wavelet analysis, regression analysis and the Mann-Kendall test, this paper analyzed time-series (1959–2006) weather
data from 23 meteorological stations in an attempt to characterize the climate change in the Tarim River Basin of Xinjiang
Uygur Autonomous Region, China. Major findings are as follows: 1) In the 48-year study period, average annual temperature,
annual precipitation and average annual relative humidity all presented nonlinear trends. 2) At the 16-year time scale, all
three climate indices unanimously showed a rather flat before 1964 and a detectable pickup thereafter. At the 8-year time
scale, an S-shaped nonlinear and uprising trend was revealed with slight fluctuations in the entire process for all three
indices. Incidentally, they all showed similar pattern of a slight increase before 1980 and a noticeable up-swing afterwards.
The 4-year time scale provided a highly fluctuating pattern of periodical oscillations and spiral increases. 3) Average annual
relative humidity presented a negative correlation with average annual temperature and a positive correlation with annual
precipitation at each time scale, which revealed a close dynamic relationship among them at the confidence level of 0.001.
4) The Mann-Kendall test at the 0.05 confidence level demonstrated that the climate warming trend, as represented by the rising
average annual temperature, was remarkable, but the climate wetting trend, as indicated by the rising annual precipitation
and average annual relative humidity, was not obvious. 相似文献
966.
Livelihood strategy change and land use change —Case of Danzam Village in upper Dadu River watershed, Tibetan Plateau of China 总被引:2,自引:1,他引:1
Land use change in rural China since the 1980s, induced by institution reforms, urbanization, industrialization and population
increase, has received more attention. However, case studies on how institution reforms affect farmers’ livelihood strategies
and drive land use change are scarce. By means of cropland plots investigations and interviews with farmers, this study examines
livelihood strategy change and land use change in Danzam Village of Jinchuan County in the upper Dadu River watershed, eastern
Tibetan Plateau, China. The results show that, during the collective system period, as surplus labor forces could not be transferred
to the secondary and tertiary industries, they had to choose agricultural involution as their livelihood strategy, then the
farmers had to produce more grains by land reclamation, increasing multiple cropping index, improving input of labor, fertilizer,
pesticide and adopting advanced agricultural techniques. During the household responsibility system period, as labors being
transferred to the secondary and tertiary industries, farmers chose livelihood diversification strategy. Therefore, labor
input to grain planting was greatly reduced, which drove the transformation of grain to horticulture, vegetable or wasteland
and decrease of multiple cropping index. This study provides a new insight into understanding linkages among institution reforms,
livelihood strategy of smallholders and land use change in rural China.
Foundation item: Under the auspices of National Natural Science Foundation of China (No. 40601006, 40471009), National Basic
Research Program of China (No. 2005CB422006) 相似文献
967.
????13??T/P???????????????????????????????????????????????????????????????????????????????????Ubari-Murzuq????????????????????????????????????????′????????????????????????С?????Ku???κ?C???ι?????????????????????????????P???????仯?????? 相似文献
968.
��Ӷ��Ѵ������ֽ�������ЧӦ 总被引:1,自引:1,他引:0
????????????????????????β??????????????1985??2006??β?????仯??????????1???????????????????????????????????????????????????????????????????????????2????????????????????????????????1?λ??????????£??????????ε?????????????????????1?γ????????仯?????3?? ????????????????仯?????????????????仯???????????????????????????? 相似文献
969.
西北干旱区近50年气候变化特征与趋势 总被引:10,自引:2,他引:10
20世纪后期全球增暖趋势越来越明显,受全球增暖的影响,西北地区的气候也将受到不同程度的影响。选取了西北干旱区1951~2000年的21个代表站点气温、降水量资料,采用趋势系数法对西北干旱区近50年气温和降水变化进行分析,找出各分区的变化趋势。结果表明:近50年西北干旱区气温呈上升趋势(0.22℃/10 a),1986年后气温明显升高;柴达木盆地和新疆北部升温较大;各季都有增温趋势,贡献最大的是秋冬两季。降水变化有增加的趋势(3.2 mm/10 a),年降水量贡献最大的是夏季;各区降水都有增加,其中新疆北部降水增加最多。西北干旱区近50年气温升高趋势是南北高,中间低;降水量增加趋势从东南向西北呈现递增的格局。 相似文献
970.
Global sea level change and thermal contribution 总被引:4,自引:0,他引:4
The global long-term sea level trend is obtained from the analysis of tide gauge data and TOPEX/Poseidon data. The linear trend of global mean sea level is highly non-umiform spatially, with an average rate of 2.2 mm year-1 in T/P sea-level rise from October 1992 to September 2002. Sea level change duc to temperature vanation (the thermosteric sea level) is discussed. The results are compared with TOPEX/Poseidon altimeter data in the same temporal span at different spatial scales. It is indicated that the ther-mal effect accounts for 86% and 73% of the observed seasonal variability in the northern and southern hemispheres, respectively. The TOPEX/Poseidon observed sea level lags behind the TSI, by 2 months in the zonal band of 40°-60° in both the northern and southern hemispheres. Systematic differences of about 1-2cm between TOPEX/Poseidon observations and thermosteric sea level data are obtained. The potential causes for these differences include water exchange among the atmosphere, land, and oceans, and some pos-sible deviations in thermosteric contribution estimates and geophysical corrections to the TOPEX/Poseidon data. 相似文献