山东荣成天鹅湖海草场大型底栖贝类时空分布研究   总被引：1，自引：1，他引：0  

刘建影  李文涛  覃乐政  张秀梅 《海洋科学》2017,41(1):113-122

为了了解天鹅湖不同微生境条件下底栖贝类的群落结构及时空分布特征,于2013年12月至2014年11月,对天鹅湖矮大叶藻区、空白区、大叶藻区边缘及其内部的底栖贝类和环境特征进行了调查。共发现15种大型底栖贝类,隶属14科15属;贝类种类组成、分布密度、生物量以及物种多样性指数在4种生境中差异显著,但均无明显的季节变化。空白区域中贝类总密度和单位面积生物量最高,大叶藻区内部最低,但矮大叶藻区和大叶藻区内部多样性指数较高。大叶藻区内部的贝类以腹足类锈凹螺、日本月华螺、刺绣翼螺等刮食者为主,而双壳贝类则更倾向于选择无海草覆盖的空白区或者海草较为稀疏的草场边缘。综合分析表明,天鹅湖底栖贝类的分布和多样性受底质特征和海草覆盖影响最为显著,同时与水深密切相关。  相似文献   

渤海及北黄海河流悬浮颗粒碳氮同位素时空分布及源解析   总被引：2，自引：0，他引：2  

于靖  张华 《海洋科学》2017,41(5):93-102

选择流入渤海和北黄海的36条主要河流为研究对象,对比了平水期、丰水期和枯水期水体中悬浮颗粒物和河流表层沉积物的碳和氮稳定同位素的地球化学特征,并对颗粒物有机质碳和氮来源进行分析。结果表明,水体悬浮有机质碳同位素总体上表现为δ13C平水期δ13C丰水期δ13C枯水期的特点,δ15N值呈δ15N丰水期δ15N平水期δ15N枯水期的特点。渤海和北黄海的主要入海河流悬浮颗粒物有机质的来源具有明显的季节性差异,悬浮颗粒有机质碳平水期(春秋季)来源以C3植物、土壤有机质和水生藻类为主,丰水期(夏季)碳的各来源中浮游植物的贡献率明显增大,枯水期(冬季)则表现为陆源C3植物分解和水源性有机质的混合来源;悬浮颗粒态氮的来源与季节性降水量、生活污水、合成化肥及河流内源性水生植物密切相关。  相似文献   

Spatiotemporal changes of cold surges in Inner Mongolia between 1960 and 2012   总被引：4，自引：4，他引：0  

Xianfeng LIU  Xiufang ZHU  Yaozhong PAN  Anzhou ZHAO  Yizhan LI 《地理学报(英文版)》2015,25(3):259-273

In this study, we analyzed the spatiotemporal variation of cold surges in Inner Mongolia between 1960 and 2012 and their possible driving factors using daily minimum temperature data from 121 meteorological stations in Inner Mongolia and the surrounding areas. These data were analyzed utilizing a piecewise regression model, a Sen+Mann- Kendall model, and a correlation analysis. Results demonstrated that (1) the frequency of single-station cold surges decreased in Inner Mongolia during the study period, with a linear tendency of -0.5 times/10a (-2.4 to 1.2 times/10a). Prior to 1991, a significant decreasing trend of -1.1 times/10a (-3.3 to 2.5 times/10a) was detected, while an increasing trend of 0.45 times/10a (-4.4 to 4.2 times/10a) was found after 1991. On a seasonal scale, the trend in spring cold surges was consistent with annual values, and the most obvious change in cold surges occurred during spring. Monthly cold surge frequency displayed a bimodal structure, and November witnessed the highest incidence of cold surge. (2) Spatially, the high incidence of cold surge is mainly observed in the northern and central parts of Inner Mongolia, with a higher occurrence observed in the northern than in the central part. Inter-decadal characteristic also revealed that high frequency and low frequency regions presented decreasing and increasing trends, respectively, between 1960 and 1990. High frequency regions expanded after the 1990s, and regions exhibiting high cold surge frequency were mainly distributed in Tulihe, Xiao’ergou, and Xi Ujimqin Banner. (3) On an annual scale, the cold surge was dominated by AO, NAO, CA, APVII, and CQ. However, seasonal differences in the driving forces of cold surges were detected. Winter cold surges were significantly correlated with AO, NAO, SHI, CA, TPI, APVII, CW, and IZ, indicating they were caused by multiple factors. Autumn cold surges were mainly affected by CA and IM, while spring cold surges were significantly correlated with CA and APVII.  相似文献   

近50年青藏高原东部降雪的时空演变   总被引：1，自引：0，他引：1  

胡豪然  梁玲 《地理学报》2014,69(7):1002-1012

选用1967-2012年青藏高原东部60个站点的观测资料,分析了该地区降雪的时空演变特征,并结合降水和气温的变化,探讨了降雪与积雪的关系,结果表明：青藏高原东部年降雪量在1.3~152.5 mm范围内变化,空间分布差异显著;秋季降雪表现出中间多、周边少的特征,冬季降雪表现出由东南向西北递减的特征,春季降雪最多且空间分布与年降雪基本一致;降雪可划分为青南高原区、藏北高原区、柴达木盆地区、青藏高原东南缘区、川西高原西北部区、青藏高原南缘区、青海东北部区及藏南谷地区;就青藏高原整体而言,除秋季外,整年、冬季和春季降雪均表现出“少—多—少”的年代际变化特征,其中冬季降雪在1986年发生了由少到多的突变,整年、冬季和春季降雪均在1997年发生了由多到少的突变;不同区域降雪的时间变化规律各具特点;降雪与积雪的关系十分密切,春季降雪受气温的影响最为显著,秋季次之,冬季最弱;20世纪末,春季降雪受气温升高的影响表现出与降水变化相反的由多到少的气候突变特征。  相似文献   

Interannual meridional displacement of the East Asian upper-tropospheric jet stream in summer   总被引：31，自引：0，他引：31  

LIN Zhong  LU Riyu 《大气科学进展》2005,22(2):199-211

On the interannual timescale, the meridional displacement of the East Asian upper-tropospheric jet stream (EAJS) is significantly associated with the rainfall anomalies in East Asia in summer. In this study, using the data from the National Centers for Environmental Prediction-Department of Energy (NCEP/DOE) reanalysis-2 from 1979 to 2002, the authors investigate the interannual variations of the EAJS‘s meridional displacement in summer and their associations with the variations of the South Asian high (SAH) and the western North Pacific subtropical high (WNPSH), which are dominant circulation features in the upper and lower troposhere, respectively. The result from an EOF analysis shows that the meridional displacement is the most remarkable feature of the interannual variations of the EAJS in each month of summer and in summer as a whole. A composite analysis indicates that the summer (June-July-August, JJA) EAJS index, which is intended to depict the interannual meridional displacement of the EAJS, is not appropriate because the anomalies of the zonal wind at 200 hPa (U200) in July and August only, rather than in June, significantly contribute to the summer EAJS index. Thus, the index for each month in summer is defined according to the location of the EAJS core in each month. Composite analyses based on the monthly indexes show that corresponding to the monthly equatorward displacement of the EAJS, the South Asian high (SAH) extends southeastward clearly in July and August, and the western North Pacific subtropical high (WNPSH) withdraws southward in June and August.  相似文献   

基于MODIS的祁连山区积雪时空变化特征   总被引：1，自引：0，他引：1  

蔡迪花  郭铌  王兴  张小文 《冰川冻土》2009,31(6):1028-1036

利用2000-2003年日资料经8 d合成的500 m分辨率MODIS卫星反演积雪资料和数字高程模型, 借助于GIS空间分析技术, 以积雪频率和积雪盖度为监测指标, 研究分析了祁连山区整体的积雪空间分布状况及其年内变化特征, 地形对积雪的分布和季节变化的影响. 结果表明: 祁连山区的积雪分布极不均匀, 积雪主要沿山系走向成条带状分布, 呈现西段多, 东段次之, 中部和南部少, 山脊多, 山谷少的特征, 且海拔越高、 山势越陡、阴坡积雪的范围越大、持续时间越久. 累积降雪时间, 就全区而言为9月至翌年5月, 但不同高度、坡度和坡向带有所差别. 海拔4 000 m以上区域存在春、秋季两个时段的积雪补给, 而海拔4 000 m以下仅有中秋至中冬一个时段的积雪补给;坡度较平缓的区域冬季和春季为主要积雪补给期, 而坡度较陡的区域则为秋季和春季;平地和南坡积雪补给主要发生在冬季和春季, 而其它坡向为春季和秋季.  相似文献   

2003—2019年邯郸市叶面积指数时空变化特征     

李武乾  张安兵  王贺封  于坤  焦月正 《测绘与空间地理信息》2022,(2):25-28

研究和掌握叶面积指数(LAI)时空变化特征,对区域植被保护、植树造林和环境保护具有重要的参考意义.本文以邯郸市为例,基于MCD15A3H遥感影像数据、DEM数据和土地利用等多元数据,引入Sen趋势与Mann-Kendall趋势检验分析方法,系统分析了邯郸市像素尺度上的LAI数值的变化特征,并基于不同的土地利用类型、不同...  相似文献   

The seasonal range of sea temperature on the New Zealand shelf   总被引：1，自引：1，他引：0  

D. M. Garner 《新西兰海洋与淡水研究杂志》2013,47(2):201-208

Sea water temperatures measured over the New Zealand continental shelf in summer and winter 1967 are compared and discussed.  相似文献   

Interannual Sea Level Variations in the South China Sea Over 1950–2009     

Dongju Peng  Hindumathi Palanisamy  Anny Cazenave  Benoit Meyssignac 《Marine Geodesy》2013,36(2):164-182

Spatial patterns of interannual sea level variations in the South China Sea (SCS) are investigated by analyzing an EOF-based 2-dimensional past sea level reconstruction from 1950 to 2009 and satellite altimetry data from 1993 to 2009. Long-term tide gauge records from 14 selected stations in this region are also used to assess the quality of reconstructed sea levels and determine the rate of sea level along the coastal area. We found that the rising rate of sea levels derived from merged satellite altimetry data during 1993–2009 and past sea level reconstruction over 1950–2009 is about 3.9 ± 0.6 mm/yr and 1.7 ± 0.1 mm/yr, respectively. For the longer period, this rate is not significantly different from the global mean rate (of 1.8 ± 0.3 mm/yr). The interannual mean sea level of the SCS region appears highly correlated with Niño 4 indices (a proxy of El Niño-Southern Oscillation/ENSO), suggesting that the interannual sea level variations over the SCS region is driven by ENSO events. Interpolation of the reconstructed sea level data for 1950–2009 at sites where tide gauge records are of poor quality (either short or gapped) show that sea level along the Chinese coastal area is rising faster than the global mean rate of 1.8 mm/yr. At some sites, the rate is up to 2.5 mm/yr.  相似文献   

Studies on twelve common bivalve larvae,with notes on bivalve spawning seasons in New Zealand     

John D. Booth 《新西兰海洋与淡水研究杂志》2013,47(3):231-265

Twelve common bivalve larvae occurring in the plankton from the Bay of Islands (35°15'S, 174°10'E), Wellington Harbour (41°16'S, 174°51'E), and off Raumati Beach (40°56'S, 174°58'E), New Zealand, during 1970–72 are described and, wherever possible, provisionally identified. The seasonal occurrences of these larvae in the plankton are also described. Information on the spawning cycles of some New Zealand adult bivalves is reviewed; although some species have a short (4 months or less) spawning season, for most it is much longer, possibly with ‘trickle’ spawning through several months of the year.  相似文献