海南岛冬季暴雨的时空分布及大尺度环流场特征分析          下载免费PDF全文

曾敏  王咏青  冯文 《气象科学》2023,43(5):589-599

利用海南岛气象观测站逐日降水整编资料和欧洲中期天气预报中心（European Centre for Medium-Range Weather Forecasts，ECMWF） ERA5再分析资料，分析了1991—2020年海南岛冬季暴雨的时空分布及环流特征。结果表明：海南岛冬季暴雨在月际分布（12月—次年2月）上存在较大差异性，降雨量级越大，差异越明显；在空间分布上也存在显著的地域性，东部地区发生频次最高，总体上呈现东多西少的分布特征。海南岛冬季暴雨的水汽输送主要以偏东方向为主，气流来自副高南侧的偏东气流和大陆冷高压东南侧的东北气流。海南岛冬季暴雨发生期间，相对气候平均态而言，偏东低空急流较为强劲，中南半岛南支槽形态明显，副高偏北偏西偏强，南亚高压西北向的出流偏强，且南海海域存在显著的海温正距平。  相似文献   

居民对海岛旅游影响感知的实证研究     

陈金华 《广东海洋大学学报》2007,27(5):20-25

采用实地考察、问卷调查与访谈的方法对我国旅游型海岛东山岛进行调查发现,当地居民对旅游影响的正面感知较强,突出表现在旅游经济影响方面,反映了当地旅游业发展处于起步阶段;居民对旅游的负面影响感知较弱,反映了当地经济转型时期居民对旅游业的期望较高;居民人口统计学的差异对旅游影响感知总体差异不大,但在某些方面存在一定差异。  相似文献   

First cosmogenic 10Be constraints on LGM glaciation on New Zealand's North Island: Park Valley,Tararua Range     

Martin S. Brook  James Shulmeister  Tyne V. H. Crow  Albert Zondervan 《第四纪科学杂志》2008,23(8):707-712

We report the first direct ages for late Quaternary glaciation on the North Island of New Zealand. Mt Ruapehu, the volcanic massif in the North Island's centre, is currently glaciated and probably sustained glaciers throughout the late Quaternary, yet no numeric ages have been reported for glacial advances anywhere on the North Island. Here, we describe cosmogenic ¹⁰Be ages of the surface layers of a glacially transported boulder and glacially polished bedrock from the Tararua Range, part of the axial ranges of the North Island. Results indicate that a limited valley glaciation occurred, culminating in recession at the end of the last glacial coldest period (LGCP, ca. 18 ka). This provides an initial age for deglaciation on the North Island during the last glacial–interglacial transition (LGIT). It appears that glaciation occurred in response to an equilibrium‐line altitude (ELA) lowering of ～1400 m below the present‐day mean summer freezing level. Ages for glaciation in the Tararua Range correspond closely to exposure ages for the last glacial maximum (LGM) from the lateral moraines of Cascade Valley in the South Island, and in Cobb Valley, in northern South Island. The corollary is that glaciation in the Tararua Range coincided with the phase of maximum cooling during MIS 2, prior to the Antarctic Cold Reversal (ACR), during the LGCP. Copyright © 2008 John Wiley & Sons, Ltd.  相似文献   

Report of Pontoniinae Shrimps (Crustacea: Decapoda) Collected by Joint Chinese-German Marine Biology Expeditions to Hainan Island, South China Sea. Ⅲ. Periclimenes     

李新正  刘瑞玉 《中国海洋湖沼学报》2004,(1)

1　INTRODUCTIONInthefirstandsecondpapersofthisseries (LietLiu ,2 0 0 2 ,2 0 0 3) ,wereported 9genera 1 6speciesofPontoniinae ,collectedbytheJointChinese GermanMa rineBiologyExpeditionstoHainanIsland (winterof1 990andspringof 1 992 ) .ThepresentpaperreportsonthespeciesofgenusPericlimenesfromHainanIslandcollectedbytheexpedition.ThematerialsstudiedherearealldepositedintheInstituteofOceanology ,ChineseAcademyofSciences,Qingdao,China (IOCAS) .Inthispaper,“Materialexamined”and“RN…  相似文献   

The deglaciation of Clyde Inlet,northeastern Baffin Island,Arctic Canada     

Jason P. Briner  Irina Overeem  Gifford Miller  Robert Finkel 《第四纪科学杂志》2007,22(3):223-232

The behaviour of ice sheets as they retreated from their Last Glacial Maximum (LGM) positions provides insights into Lateglacial and early Holocene ice‐sheet dynamics and climate change. The pattern of deglaciation of the Laurentide Ice Sheet (LIS) in arctic fiord landscapes can now be well dated using cosmogenic exposure dating. We use cosmogenic exposure and radiocarbon ages to constrain the deglaciation history of Clyde Inlet, a 120 km long fiord on northeastern Baffin Island. The LIS reached the continental shelf during the LGM, retreated from the coastal lowlands by 12.5 ± 0.7 ka (n = 3), and from the fiord mouth by 11.7 ± 2.2 ka (n = 4). Rapid retreat from the outer fiord occurred 10.3 ± 1.3 ka (n = 6), with the terminus reaching the inner fiord shortly after 9.4 ka (n = 2), where several moraine systems were deposited between ca. 9.4 and ca. 8.4 ka. These moraines represent fluctuations of the LIS during the warmest summers since the last interglaciation, and this suggests that the ice sheet was responding to increased snowfall. Before retreating from the head of Clyde Inlet, the LIS margin fluctuated at least twice between ca. 7.9 and ca. 8.5 ka, possibly in response to the 8.2 ka cold event. Copyright © 2006 John Wiley & Sons, Ltd.  相似文献   

CHEMICAL CHARACTERISTICS OF THE COASTAL SEA OFF TIANHENG ISLAND   总被引：1，自引：0，他引：1  

徐明德 《中国海洋湖沼学报》1994,12(3):228-235

Chemical characteristics of the coastal sea off Tianheng Island were investigated from May 1990 toFebruary 1991 in this study which included distribution pattern,seasonal variability and the controlling fac-tors of oxygen,pH,nutrients.The rich nutrient salt content is suited for phytoplankton growth andmariculture.The coastal sea waters is of good quality based on the national standard of seawater qual-ity in terms of pH,oxygen,and nutrients,the main controlling factors for which in the investigated seaarea are hydrographic(salinity,temperature,river runoff,etc.),biological(photosynthesis of plankton),andanthrogenic(fertilizing in the nearby land and sea).  相似文献   

南极乔治王岛菲尔德斯半岛西湖柱状剖面藻类化石与环境演变          下载免费PDF全文

刘清泗  降廷梅 《极地研究》1990,2(2):28-35

根据西湖柱状岩芯样品中藻类化石的分布与含量变化,推测本区在3600年前仍为冰川覆盖;距今3600～3000年前为冰缘浅湖期;3000～1200年前湖水稳定,气候环境相对较好;距今1200年至现代气候略有波动。  相似文献   

The benthic macroinvertebrates of the Block Island Sound     

Frank W. Steimle 《Estuarine, Coastal and Shelf Science》1982,15(1):1-16

The benthic invertebrates of Block Island Sound have not been adequately studied, in contrast to other adjacent southern New England sounds. This study examines the species composition, abundance and biomass of benthic macrofaunal invertebrates at nine locations within Block Island Sound. The sites sampled, represent a wide range of subtidal habitats within the Sound, and were visited in February and September.Some 224 species were identified, of which almost half (104) were polychaetes. The benthic assemblages at most stations were dominated numerically by tube dwelling, surface detritus or suspension feeding amphipods, e.g. Ampelisca agassizi and A. vadorum, as well as the protobranch bivalve, Nucula proxima. This dominant Ampelisca-Nucula assemblage was associated with silty fine sand sediments. The average macrofaunal biomass for all stations was 158 g (wet weight) m^?2, two thirds the average benthic biomass of Georges Bank, an important fishery area. Based on the examination of the records of earlier surveys in Block Island Sound, there is evidence that this silty-sand, ampeliscid-dominated assemblage has persisted since at least the mid-1940s.  相似文献   

南极乔治王岛的地理环境分析：兼论南极地缘政治问题   总被引：1，自引：0，他引：1  

朱诚  陈传康 《地理学报》1991,46(3):300-309

作者从地理环境,尤其是气候和资源对航空、航海、科学考察的影响,讨论了南极乔治王岛地区的战略意义。根据对地质基础、矿产、火山活动以及冰川侵蚀历史和地貌现象的讨论,指出该区是研究古气候、古环境、大陆漂移和冰川冰缘地貌的极好场所;并指出该区种类全、数量多且具有南极特征的动植物和奇特的食物链关系,是其成为重要生物资源区和受条约保护的特别科学兴趣场所的主要原因;最后讨论了本区归属问题,认为《南极条约》今后可能继续生效或会制定出类似条约使本区和南极继续成为全人类的共有财富。  相似文献   

海南岛长昌盆地始新世孢粉植物区系     

赵炜  沈如江  廖文波  金建华 《吉林大学学报(地球科学版)》2009,39(3):379-385

海南岛长昌盆地始新世孢粉植物区系共计种子植物32科40属,蕨类植物8科11属。分析其中的种子植物区系成分并与海南岛现代植物区系进行对比,结果显示：（1）在科级水平,长昌盆地始新世孢粉植物区系以泛热带科占优势,为37.5%;热带-亚热带科占6.25%;而亚热带-温带科所占比例相对较高,达到31.25%。海南岛现代植物区系泛热带科高达48.07%,热带-亚热带科的比例也达到18.88%,而亚热带-温带科仅占15.88%。显然,长昌盆地始新世植物区系的组成亚热带性质较强。（2）在属级水平,长昌盆地始新世孢粉植物区系泛热带属占7.5%;热带-亚热带属占17.5%;而亚热带-温带属多达67.5%。海南岛现代植物区系泛热带属高达23.9%,热带-亚热带属更是高达57.5%,而亚热带-温带属仅占13.7%。对比表明,长昌盆地始新世植物区系明显以亚热带-温带性质为主,甚至出现了很多现今生活在较高海拔的山地植物,如冷杉（Abies）和铁杉（Tsuga）等。科属组成的分析表明,海南岛长昌盆地始新世的气温比现代要低,其周缘地带很可能分布有较高的山地。  相似文献