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891.
892.
Vertical profiles of temperature and salinity have been measured for 50 years along Line P between the North American west coast and mid Gulf of Alaska. These measurements extend 1425 km into the gulf at 13 or more sampling stations. The 10-50-m deep layer of Line P increased in temperature by 0.9 °C from 1958 to 2005, but is significant only at the 90% level due to large interannual variability. Most of this increase in temperature accompanies the 1977 shift in wind patterns. Temperature changes at 100-150 m and salinity changes in both layers are not statistically significant. Much of the variance in temperature is in the upper 50 m of Line P, and temperature changes tend to be uniform along Line P except for waters on the continental margin. Salinity changes are dominated by variability in the halocline between 100 and 150 m depth and are less uniform along Line P. Largest oscillations in temperature and salinity are between 1993 and 2003. These events can be understood by considering changes in eastward wind speed and wind patterns that are revealed in the first two modes of the Pacific Decadal Oscillation. Changes in these patterns are indicators for both Ekman surface forcing (Surface ocean currents flow to the right of the wind direction) and Ekman pumping (Surface waters diverge away from regions of positive wind stress curl, leading to upwelling of colder saltier water). Changes in temperature along the nearshore part of Line P suggest Ekman surface forcing is the stronger of the two processes in the upper layer. The change in salinity anomalies in the halocline along the seaward end of Line P, following the wind shift in 1977, is in agreement with enhanced upwelling caused by stronger Ekman pumping in this region. 相似文献
893.
1 INTRoDUcTIONThe study results from Nov. 1986 to Aug. 1990 in sea area (ll5"E - 165"E, 20"N -l0"S) during TOGA experiments, indicated that there were outstanding responses of differenceof partial pressure of CO, between sea and air (APCO,) and total dissolved concentrationof CO, (TCO,) to El Nino and La Nina in NW region of the Western Tropical Pacific,including the cruise lines from ll4ofy 22"N to l30"E, l8"N and that from l8"N to 8"N,along l30"E. The characteristics of dis… 相似文献
894.
主要研究了菲律宾东南海域(区域I)和伊里安岛东部的北部海域(区域Ⅱ)上层水(0~150m)化学参数pH,Eh,Es,∑S(-Ⅱ)和a^2-s等的分布特征和-2价硫的产生机制,结果表明,该海域表层南赤道逆流和次表层的赤道潜流是影响化学参数特别是DO和∑S(-Ⅱ)的主要因素,高生产力与高水温是赤道西太平洋上层水中-2价硫产生与保存的重要影响因素,区域Ⅱ中的pH,∑S(-Ⅱ)a^2-s,DO比区域I高而 相似文献
895.
896.
PeriodcomponentsinthemonthlymeansealevelvariationsinthePacificOcean¥TianSuzhen;MaJirui;ZhengWenzhen;ChaiXinminandZhangQin(Rec... 相似文献
897.
本文根据1985—1988年4次考察中140°E断面的温、盐度和海流资料指出,由于1986—1987年E1 Ni(?)o事件的出现,因而原先积聚在西太平洋赤道海域的上层暖水减少,次表层水和中层水显著抬升,从而改变了热带海域的温、盐度场结构。此外,南赤道流几乎消失以及赤道潜流核心层速度的明显减弱,是这次E1 Ni(?)o事件造成的海流方面的重要变化。结合1982—1983年E1 Ni(?)o事件爆发前137°E断面表层动力高度的分布变化,可初步认为西太平洋赤道海域已具备了产生下一次E1 Ni(?)o事件的海洋学条件。 相似文献
898.
福建太平洋牡蛎种群微卫星DNA分析 总被引:1,自引:0,他引:1
本文采用Ucdcg153、157、202微卫星引物对福建两个太平洋牡蛎(学名为长牡蛎Crassostrea gigas)养殖种群进行扩增分析和序列测定.与采自漳浦旧镇的近江牡蛎(C. ariakensis)比较,前者对以上三种引物全部呈阳性反应,后者只对Ucdcg157显阳性.与Genebank提供的相关序列比较,福建太平洋牡蛎与Genebank样品应属同源,其中漳浦霞美和厦门白礁的样品则可能代表同一种群的两个衍生品系.本项调查结果同时显示,近亲繁殖的育苗方式已经导致福建太平洋牡蛎种群裂化;任其发展不利于维护良种优势.本次采集的样品中未发现显示葡萄牙牡蛎、熊本牡蛎和美洲牡蛎微卫星特征的个体. 相似文献
899.
李文勤 《中国海洋大学学报(自然科学版)》1989,(4)
本文通过对中太平洋北部海盆表层和柱状沉积物中钙质超微化石的分析鉴定,讨论了该调查区处在溶跃面以下表层沉积物中钙质超微化石的种数与水深变化的关系,推测出本调查区中Ⅰ区的碳酸盐补偿深度约5300米。根据地层中出现的标准化石,对柱状岩芯M_(14)进行了地层年代划分。最上部地层年代约为27万年前,向下1米处年代约为44万年前,3.66米处年代约为122万年前。 相似文献
900.
Hajime Kawakami Makio C. Honda Masahide Wakita Shuichi Watanabe 《Journal of Oceanography》2007,63(6):967-982
Time-series measurements of dissolved inorganic carbon (DIC) and nutrient concentrations were conducted in the northwestern
North Pacific from October 2002 to August 2004. Assuming that data obtained in different years represented time-series seasonal
data for a single year, vertical distributions of DIC and nutrients showed large seasonal variabilities in the surface layer
(∼100 m). Seasonal variabilities in normalized DIC (nDIC) and nitrate concentrations at the sea surface were estimated to
be 81–113 μmol kg−1 and 12.7–15.7 μmol kg−1, respectively, in the Western Subarctic Gyre. The variability in nutrients between May and July was generally at least double
that in other seasons. In the Western Subarctic Gyre, estimations based on statistical analyses revealed that seasonal new
production was 39–61 gC m−2 and tended to be higher in the southwestern regions or coastal regions. The seasonal new productions in the northwestern
North Pacific were two or more times higher than in the North Pacific subtropical gyre and the northeastern North Pacific.
It is likely that this difference is due to spatial variations in the concentrations of trace metals and the species of phytoplankton
present. In addition, from estimations of surface pCO2 it was verified that the Western Subarctic Gyre is a source of atmospheric CO2 between February and May and a sink for CO2 between July and October. 相似文献