华南夏季降水与全球海温的关系   总被引：14，自引：4，他引：14  

徐海明 《南京气象学院学报》1997,20(3):392-399

用１９５４￣１９８９年华南夏季（６￣７月）降水资料和全球月平均海温资料作了简单的相关分析。分析结果表明，华南夏季降水与前期冬季１月的黑潮海温存在显著的负相关，冬季１月黑潮异常增暖有利于华南夏季干旱的产生，而异常偏冷则有利于洪涝的产生。计算结果进一步表明，华南夏季降水与菲律宾、台湾一带的海温以及北大西洋中纬度海温在整个前期春季、同期夏季存在显著的负相关，意叶着以上两海区海温在春夏异常增暖有利于华南夏  相似文献   

厄尔尼诺事件对黑龙江省低温洪涝灾害的影响及其预报   总被引：2，自引：0，他引：2  

魏松林 《黑龙江气象》2001,(2):27-31

在研究厄尔尼诺（拉尼娜）事件对黑龙江省低温洪涝灾害影响的基础上，提出一种表征厄尔尼诺的指数（ENI）。根据ENI谱分析结果，提出了一种厄尔尼诺事件和拉尼娜事件的统计预测方法。经1997年对强厄尔尼诺和1998年对拉尼娜事件预报检验证明，该方法可行，可在区域和省级短期气候预测中应用。  相似文献   

High-resolution records of thermocline in the Okinawa Trough since about 10000 aBP     

Wang Jiliang  SAITO Yoshiki  OBA Tadamichi  JIAN Zhimin  WANG Pinxian 《中国科学D辑(英文版)》2001,44(3):193-200

The present paper uses planktonic foraminifera and their stable isotopes to study the changes in the depth of thermocline (DOT) in the Okinawa Trough since the last 10000 a based on the analysis of Core B-3GC in the northern Okinawa Trough, together with that of the core in the southern Okinawa Trough. As results show, the thermocline was shallow before 6400 aBP, and deepened afterward, then became shallow again from 4000 to 2000 aBP. The DOT fluctuations display a positive correlation with those of sea surface temperature (SST). In addition, the changes in the northern Okinawa Trough are similar to those in the southern trough, implying a possible connection with the variation of the Kuroshio Current. The changes of SST and DOT suggest that the Kuroshio Current changed its intensity or main axis from 4000 to 2000 aBP and around about 6400 aBP respectively. Moreover, the changes of DOT from 8200 to 6400 aBP may indicate a gradual intensification of the Kuroshio Current.  相似文献   

NUMERICAL EXPERIMENTS FOR CLIMATE VARIABILITY OF MONSOON UNDER THE UNITED EFFECTS OF ANTARCTIC ICE COVER AND SEA SURFACE TEMPERATURE   总被引：1，自引：0，他引：1  

陈隆勋  缪群 《Acta Meteorologica Sinica》1996,(4)

In order to study the mechanisms of climate natural variability under the united effects of antarc-tic ice cover(AIC)and sea surface temperature(SST),we have done a series of numerical experi-ments for the climate variability of the period from January 1981 to December 1983 by using a three-level atmospheric general circulation model(AGCM).Firstly we conduct climate integration for sixyears,then 3 years'control integration from January 16 of the seventh year.Moreover,we do threesensitivity experiments,which are the sensitivity experiments forced by observed SST and AIC.ob-served SST and climatic AIC,observed AIC and climatic SST respectively,to study the climate vari-ability and its mechanisms affected by SST and AIC.We put emphasis on the variability of East Asiamonsoon and the Southern Hemisphere(SH)circulation.In this paper,introduction is made to theresults of control test and the sensitivity experiment forced by observed SST and AIC,and the pre-dictability of the monsoon climate variability is discussed.  相似文献   

Influences of the extratropical pacific sst on the precipitation of the north china region     

Geng Quanzhen  Ding Yihui  Huang Chaoying 《大气科学进展》1997,14(3):339-349

The influences of the extratropical Pacific SST on the precipitation of the North China region are reexamined with the observational data and studied with numerical simulations by using NCAR CCM2. It is found that there ex-ist high positive correlations between the annual precipitation of the North China region and the extratropical Pacific SST in late spring, especially in two regions, e.g., the Kuroshio Current region and the midlatitude central Pacific re-gion. The numerical simulations with NCAR CCM2 show that the warmer SSTs in the Kuroshio Current region and the midlatitude central Pacific in late spring can generate a large-scale circulation pattern over the Asia-Pacific re-gion that is favorable to the precipitation of the North China region.  相似文献   

南海表层水温低频振荡的基本特征   总被引：24，自引：3，他引：24  

于慎余  周发琇  傅刚  王东晓 《海洋与湖沼》1994,25(5):546-551

使用１９５８－１９８７年ＣＯＡＤＳ资料对南海全区表层水温做了分析。结果发现，南海表层水温存在２０－４０个月的低频振荡，其中以准两年周期最显著，其次是３－４年，这种振荡主要发生在深水海盆区，并且与季风异常有着十分密切的关系。  相似文献   

西太平洋暖池海域SST场的时空特征   总被引：7，自引：3，他引：7  

张启龙  翁学传  颜廷壮 《海洋与湖沼》2001,32(4):349-354

根据 1 950— 1 998年间月平均SST资料 ,用经验正交函数 (EOF)分析法 ,对西太平洋暖池海域SST场的时空特征进行了分析。结果表明 ,暖池海域SST场的主要模态包括年、年际和年代际变化 3个类型 ,其主要变化周期依次为 1 2、54、2 9和 1 2 0个月 ;暖池SST场的年际变化具有明显的区域性 ,全海域大致以 1 60°E为界分为东、西两部分 ,其SST的年际变化在变幅、相位和周期方面存在着明显差异。  相似文献   

热带西太平洋海水热结构对1986—1987年ENSO事件的响应     

刘赞沛 《海洋与湖沼》1992,23(1):14-19

本文利用热带西太平洋中、美海气第1至第4航次联合考察资料,分析讨论了1986—1987年El Ni(?)o/Southern Oscillation(ENSO)事件期间该区热结构的变化。分析表明,事件期间热带西太平洋暖水域海水热含量显著降低,它与140°W和Nino_1+Nino_2区的SST距平变化恰成反位相关系。此外,温跃层在此期间内上升了50—100m,上混合层明显变浅。这种温跃层的异常上升是与事件期间此区西风异常的出现和赤道两侧正的风应力旋度增大有着密切关系。  相似文献   

Anticyclonic Eddy Revealing Low Sea Surface Temperature in the Sea South of Japan: Case Study of the Eddy Observed in 1999–2000     

Kohtaro Hosoda  Kimio Hanawa 《Journal of Oceanography》2004,60(4):663-671

Various kinds of datasets, such as satellite-derived sea surface temperature (SST), sea surface height, surface velocity produced by combining surface drifter and satellite altimeter data, and hydrographic data, led to the discovery of an anticyclonic eddy with lower SST than those of surrounding waters in the Kuroshio recirculation region south of Shikoku, as if the eddy were cyclonic. This anticyclonic eddy was formed east of Kyushu in late August to early September 1999 from the merger of two anticyclonic eddies which had migrated in the recirculation region to the sea south of Japan from the east. After the merger, the anticyclonic eddy strengthened abruptly and began to exhibit the low SST. In October, this eddy coalesced with the Kuroshio and moved swiftly eastward, accompanied by an amplitude growth of the Kuroshio meander. In mid November, off the Kii Peninsula, the eddy detached from the meandering Kuroshio. It then moved southwestward and again slowly propagated westward along the 30°N line. During this period, at least from late October 1999 to January 2000, SSTs over the anticyclonic eddy were found to be continuously lower than those of surrounding waters. This case tells us that we have to pay careful attention to the interpretation of mesoscale SST distributions. This revised version was published online in July 2006 with corrections to the Cover Date.  相似文献   

Interannual variations of the occurrence of epipelagic fish in the diets of the seabirds breeding on Teuri Island, northern Hokkaido, Japan     

Tomohiro Deguchi  Yutaka Watanuki  Yasuaki Niizuma  Akifumi Nakata 《Progress in Oceanography》2004,61(2-4):267

The diets of breeding seabirds can be a good monitor of marine environmental changes. From 1984 to 2001 we monitored the diets of black-tailed gulls (Larus crassirostris) (“surface foragers”), rhinoceros auklets (Cerorhinca monocerata) (“epipelagic divers”), and Japanese cormorants (Phalacrocorax filamentotus) (“bottom divers”) that breed on Teuri Island at the northern boundary of the Tsushima Warm current in the Sea of Japan/East Sea. Between 1984 and 1987, both the gulls and the auklets foraged on the sardine (Sardinops melanostictus), but after 1992, they switched to the anchovy (Engraulis japonica). This change might reflect the collapse of the sardine stock in the late 1980s. In the 1990s, the year-to-year variations of the percentage of anchovy in the diets of the three seabird species showed similar trends: High in 1994 and 1998–2001; and low in 1992–1993 and 1995–1997. The estimated stock size of the anchovy population in the Tsushima Current area was positively correlated with the percentage of mass of anchovy in the seabirds’ diets. Thus, the short-term annual changes of the total anchovy availability, which might reflect SST or the volume transport of Tsushima Current, possibly affected the seabirds diets on this island.  相似文献