OOPC海洋气候观测面板raybet雷竞技最新

1997:海平面报告的国际研讨会。NOAA (GCOS 43号报告,美好的55号和ICPO报告没有。16),133页。[7.4]

OOPC (海洋观测系统开发小组),1993:临时设计海洋全球气候观测系统的组件。raybet雷竞技最新德州农工大学学院站,TX 105页。[7.4]OOPC(海洋观测系统开发小组),1995:科学设计全球海洋观测系统的通用模块和全球气候观测系统:海洋气候观测系统。raybet雷竞技最新德州农工大学学院站,TX, 265页。[7.4]

支持阿,A.H.和摩根大通(J.P. Peixoto, 1983:来自观察全球角动量和能量平衡的需求。放置“。25日,355490年。[6.2]

奥尔,J。,e . Maier-Reimer Mikolajewicz et al ., 2001:人为碳吸收量的估计从四个3 d全球海洋模型。水珠。Biogeochem。周期(接受)。[6.3]《a . H。第三,t·w·惠特沃思和w·d·Nowlin Jr .) 1995:在经向南极绕极流的范围和领域。深海研究》42岁,641 - 673。[4.6,4.7]《A.H.,G.C.约翰逊和J.L. Bullister 1999:循环、混合和生产的南极底层水。掠夺。Oceanogr。43岁,55 - 109。[4.6,5.8]

奥斯本,T.J.,,投资者·布里法S.F.B.邰蒂,P.D.琼斯和r . m .小麦1999:北大西洋涛动的评价由耦合气候模型模拟。raybet雷竞技最新raybet雷竞技最新气候动力学。685 - 702。[7.3]奥斯本,顶替1980:估计当地的扩散速率从损耗测量。期刊。Oceanogr。83 - 89。[4.2,5.2]奥斯本,顶替,1988:签名双扩散对流和湍流的侵入性的政权。期刊。 Oceanogr. 18, 146-155. [5.2] Osborn, T. R. and C. S. Cox, 1972: Oceanic fine structure. Geophys. Fluid Dyn. 3, 321-345. [5.2] 0sterhus, S. and T. Gammelsrod, 1999: The abyss of the Nordic Seas is warming. J. Climate 12, 32973304. [7.3]

0 sterhus,年代。汉森,B。、Kristiansen、r和p . Lundberg 1999:通过罗银行渠道溢出。第35 - 37国际WOCE通讯,35号,WOCE国际项目办公室(未发表的文件)。[5.6]Ostlund, H.G. C.G.H. Rooth, 1990:北大西洋氚和放射性碳瞬变1972 - 1983。j .地球物理学。研究》95年,20147 - 20165。[2.1]欧文斯,b和b·a·沃伦2000:深循环在太平洋的西北角落。深海II》(新闻)。[4.5]Pacanowski司令部,1995:MOM2 Documentation, User's Guide and Reference Manual. Technical Report 3, GFDL Ocean Group Technical Report. NOAA/地球物理流体动力学实验室,普林斯顿,纽约。[5.2]Pacanowski司令部和S.G.H.调情,1981:参数化的垂直混合热带海洋的数值模型。期刊。Oceanogr。11日,1443 - 1451。[4.3,7.2]Padman、l、t·m·狄龙1987:垂直通量在波弗特海温盐楼梯。j .地球物理学。研究》92年,10799 - 10806。[5.2]Paduan, J.D. P.P. Niiler, 1993:结构在东北太平洋的速度和温度测量与拉格朗日漂流者在1987年秋季。期刊。Oceanogr。23日,585 - 600。 [4.1] Paillet, J. and M. Arhan, 1996: Shallow pycnocline and mode water subduction in the eastern North Atlantic. J. Phys. Oceanogr. 26, 96-114. [5.3] Park, K., 1969: Oceanic CO2 system: an evaluation of ten methods of investigation.Limnol。Oceanogr。14日,179 - 186。[6.3]公园,中州。和1995 l . Gamberoni:大气环流及其变化在南印度洋TOPEX /海神波塞冬altime-try。j .地球物理学。研究》100年,24911 - 24929。[3.3]公园,中州。l . Gamberoni大肠Charriaud, 1993:额叶结构,水质量,和循环海克罗泽盆地。j .地球物理学。98号决议1236112385。[4.6]

帕克,m E。r·l·斯图尔特,d . l . Farless d·e·卡特赖特,1987:一个高程卫星在轨道的选择研究海洋环流和潮。j .地球物理学。92号决议1169311707。[3.3]

高潮,G。答:拉文,h·布莱登带领一个m·加西亚和r·米勒德1994:亚热带大西洋北部的气温上升在过去35年。369年自然,48-51。[1.2,7.3]Pazan,大肠和p . p . Niiler 2000:复苏的近地表速度undrogued流浪者。j .海洋大气压。抛光工艺。(印刷中)。[4.1]Pedlosky, J。1987:一个惯性理论赤道潜流。期刊。Oceanogr。17日,19781985。[4.3,4.4]Pedlosky, J。1987 b:地球物理流体动力学,第二版。斯普林格出版社,纽约,710页(3.3,4.1,4.2)Pedlosky, J。1988年:赤道潜流的夹带和终止。期刊。Oceanogr。18日,880 - 886。[4.4]

Pedlosky, J。,1991:西部边界之间的联系当前和赤道潜流。期刊。Oceanogr。21日,1553 - 1558。[4.3]Pedlosky, J。,1996:海洋环流理论。斯普林格出版社,柏林,453页。(1.2,2.1,4.2,5.3)

Pedlosky, j·p·罗宾斯,1991:有限的角色混合层厚度结构的通风温跃层。期刊。Oceanogr。21日,10191031。[7.3]

Pedlosky, j . r .鑫黄,1999:气候强迫通风的温跃层。(提交)。[7.3]Peixoto, j·a·奥尔特,1992:物理气候。raybet雷竞技最新

美国物理研究所,纽约,520页。[4.7]珀尔帖w·R。,1998:冰河期的变化程度的大海:气候动力学和影响solidearth物理。raybet雷竞技最新启“。36岁,603 - 689。[1.2]彭,张茵。r . Wanninkhof j·l·Bullister r·a·费利和t .高桥,1998:量化的年代际人为二氧化碳吸收海洋中基于溶解无机碳的测量。大自然396年,560 - 563。[6.3]Perigaud, C。1990:海平面振荡观察地质卫星沿太平洋北赤道的两个剪切方面反向电流。j .地球物理学。研究》95年,7239 - 7248。[3.3]Perigaud、c和p . Delecluse 1992:年度海平面变化在南方热带印度洋从地质卫星和浅水模拟。j .地球物理学。研究》97年,20169 - 20178。[3.3]佩里,G。P.B.达菲和N.L.米勒,1996:扩展的数据集河排放环流模型的验证。j .地球物理学。研究》101年,21339 - 21349。[6.3]彼得斯,H。哈默,格雷格和J.M. Toole, 1988:赤道湍流参数化的。j .地球物理学。研究》93年,1199 - 1218。[4.3]彼得斯,H。桑福德,贝拉格雷格和结核,1995:赤道湍流参数化的:能细微变化的影响低于昼夜循环的范围。j .地球物理学。 Res. 100, 1833318348. [4.3]

彼得森,r·g和l . Stramma 1991:上层环流在南大西洋。掠夺。Oceanogr。26日,1 - 73。[4.3]彼得森,R.G.和w·b·白,1998:缓慢的海洋远程并置对比连接南极绕极波与热带厄尔尼诺南方涛动。j .地球物理学。研究》103年,24573 - 24583。波图霍夫(3.3,4.6,4.7),V。,a . Ganopolski诉Brovkin et al ., 2000: CLIMBER-2:中间的气候系raybet雷竞技最新统模型的复杂性。第一部分为目前的气候模型描述和性能。raybet雷竞技最新raybet雷竞技最新气候动力学。16 - 17。 [2.3]

调情,S.G.H.1986年:1984年在热带大西洋不寻常的条件。大自然322年(6076),236 - 238。[4.3]调情,S.G.H.1990年:厄尔尼诺、拉尼娜现象和南方振荡。学术出版社,圣地亚哥,CA 293页。(1.2,2.3,4.3)调情,S.G.H. Pacanowski司令部,1980:生成赤道洋流。j .地球物理学。研究》85年,1123 - 1136。[4.3]调情,S.G.H. Paconowski司令部,1986:季节性周期的模型在热带大西洋。j .地球物理学。研究》91年,14192 - 14206。[4.3]菲利普斯和S.R. Rintoul阁下2000:艾迪可变性和能量从南极绕极流的直流测量南澳大利亚。期刊。Oceanogr。3050 - 3076。[4.6]菲利普斯O.M., 1977: The Dynamics of the Upper Ocean, 2nd edn. Cambridge University Press, NY, 336 pp. [5.2]

Picaut, j . r . Tournier, 1991: 1979 - 1985监控赤道太平洋与一次性深海温度测量器数据传输。j .地球物理学。研究》96年,3263 - 3277。[4.3]Picaut, J。m . Ioulalen, t . Delcroix m . j . McPhaden和c .门克斯1996:太平洋暖池的纬向位移机制:对ENSO的影响。274年科学,1486 - 1489。[4.3]Picaut, J。f和y duPenhoat, 1997: advective-reflective ENSO的振荡性质的概念模型。277年科学,663666。[3.3]

Pickart, r S。1988:夹带和homogeniza-tion被动示踪的环流数值模型。j .地球物理学。研究》93年,6761 - 6773。[5.5]Pickart, r S。1992:水质量组件深处的北大西洋西部边界电流、深海研究》39,1553 - 1572。[5.8]Pickart R.S.、高家俊Smethie, Jr .) 1993:怎样深的西部边界电流穿过墨西哥湾流?期刊。Oceanogr。23日,26022616。[5.8]

Pickart R.S.、高家俊Smethie, 1998:深当前西部边界的演化进入亚热带域。深海研究》我45岁,1053 - 1083。[4.5]Pickart, r S。:霍格和w·m·Smethie Jr .) 1989:确定深西部边界电流的强度使用chlorofluo-romethane比率。期刊。Oceanogr。19日,940 - 951。[5.8]

Pickart, r S。,w . m . Smethie Jr . j . r . n .懒e·p·琼斯和w·j·詹金斯1996:新形成的漩涡上拉布拉多海的水。j .地球物理学。研究》101年,20711 - 20726。[5.8]

Pickart R.S.,硕士碎裂和J.R.N.懒,1997:中深通风在西部边界sub-polar环流的现行体制。深海研究》44岁,1025 - 1054。[5.4]Pickart R.S.,D.J.托雷斯和克拉克,2000:水文学拉布拉多海的对流活动。期刊。Oceanogr。(提交)。[5.5]Pickart R.S.k .薰衣草G.W.K.摩尔,f·斯特拉内奥J.R.N.懒和硕士碎裂,2000 b:拉布拉多海的水形成Irminger盆地? Deep-Sea Res. (submitted). [5.5] Pierce A.F. and B.F. Phillips, 1988: ENSO events, the Leeuwin Current and larval recruitment of the western rock lobster. J. Cons. Int. Explor. Mer, 45(1), 13-21. [1.2] Pierce, S.D., J.A. Barth and R.L. Smith, 1999: Improving acoustic Doppler current profiler accuracy with wide-area differential GPS and adaptive smoothing of ship velocity. J. Atmos. Oceanic Technol. 16, 591-596. [3.1] Pierce, S. D., R. L. Smith, P. M. Kosro, J. A. Barth and

c·d·威尔逊,2000:连续性的向南极的暗流在中纬度北太平洋的东部边界。深海研究》811 - 829页。[1.2]

Pinkel、r和s·安德森,1997:剪切、应变,理查森数变化的温跃层。第一部分:统计描述。期刊。Oceanogr。27日,264 - 281。[5.2]Pinkel、r和s .安德森,1997 b:剪切、应变,理查森数变化的温跃层。第二部分:混合建模。期刊。Oceanogr。27日,282 - 290。[5.2]Pinkel, r . j . a . Smith 1992:重复序列编码提高了多普勒声波和声雷达的精度。j .大气压。 Oceanic Technol. 9, 149163. [3.1]

d·西格尔和l·沃什伯恩1997:孤波在赤道太平洋西部。地球物理学。卷。24日,1603 - 1606。[4.3]

平克,r·t·拉兹洛,1992:太阳辐照表面建模的卫星应用在全球范围内。j:。流星。31日194 - 211。[3.4]

Piola, a和d·t·格奥尔基1982:环极的属性南极中间水和亚南极的模式。深海研究》29日687 - 711。[4.6,5.4]Piola, a和a·l·戈登,1984:太平洋和印度洋上层盐度预算。期刊。Oceanogr。747 - 753。[4.7]Piola, a和a·l·戈登,1986:海洋和淡水热通量在30°S。期刊。Oceanogr。2184 - 2190。[4.7]

Piola, a和a·l·戈登,1989:中间水在南大西洋西南部。深海36号决议论文。庄园主匹塔克(4.6)学士1978:一个关键看长期sun-weather关系。启“。空间物理。400 - 420。[2.1]Plahn o . m .大黄酸,1998:测量和建模的氯氟化碳的分布低NADW圭亚那地区盆地。j .地球物理学。研究》103年,2831 - 2848。[5.8]泊松,a,比较温度,1987:为什么会有一些人为二氧化碳在南极底层水吗? Deep-Sea Res. 34, 1255-1275. [6.3] Poisson, A., F. Culkin and P. Ridout, 1990: Inter-comparison of total alkalinity and total inorganic carbon determinations in seawater. UNESCO Technical Papers in Marine Science, UNESCO, Paris, No. 59, 18 pp. [6.3] Polito, P. S. and P. Cornillon, 1997: Long baroclinic Rossby waves detected by TOPEX/POSEIDON. J. Geophys. Res. 102, 3215-3235. [3.3] Pollard, R.T. and J. Read, 1989: A method of calibrating shipmounted acoustic doppler profilers and the limitations of gyro compasses. J. Atmos. Oceanic Technol. 6, 859-865. [3.1] Pollard, R.T., M.J. Griffiths, S.A. Cunningham, J.F. Read, F.F. Perez and A.F. Rios, 1996: Vivaldi 1991 - A study of the formation, circulation and ventilation of Eastern North Atlantic Central Water. Prog. Oceanogr. 37, 167-192. [5.4] Polovina, J.J., G.T. Mitchum and G.T. Evans, 1995: Decadal and basin-scale variation in the mixed layer depth and the impact on biological production in the Central and North Pacific, 1960-88. Deep-Sea Res I 42, 1701-1716. [1.2] Polzin, K., 1996: Statistics of the Richardson number: mixing models and fine structure. J. Phys. Oceanogr. 26, 1409-1425. [4.3] Polzin, K., 1999: A rough recipe for the energy balance of quasi-steady internal lee waves. In: 'Aha Huliko'o Proceedings Hawaiian Winter Workshop. Dynamics of Oceanic Internal Gravity Waves, P. Muller and D. Henderson (eds), Honolulu, HI, pp. 117-129. [5.2] Polzin, K., 2000: Abyssal mixing: Inertial subrange solution for the energy balance of the finescale内部波字段。j . 3月》(提交)。[5.2]

Polzin, k . l . e .射击,1997 b:估计diapy-cnal混合使用LADCP和从i8 CTD数据。39-42国际WOCE简报,不。29日,WOCE国际项目办公室。(未发表的文件)。[3.1,5.2]Polzin K.L.,J。M. Toole and R.W. Schmitt, 1995: Finescale parameterizations of turbulent dissipation. J. Phys. Oceanogr. 25, 306-328. [5.2]

Polzin, k . L。k·g·斯皮尔,j . m . Toole前作空。施密特,1996:南极底层水的强烈混合赤道大西洋。380年自然,54-57。[5.2]Polzin K.L.,J。M. Toole, J.R. Ledwell and R.W. Schmitt, 1997: Spatial variability of turbulent mixing in the深海海洋。276年科学,93 - 96。(4.2,4.6,5.2,7.2)Polzin, k . L。、大肠Kunze j . Hummon和大肠解雇2000:finescale响应的降低了ADCP速度概要文件。j .大气压。海洋抛光工艺。(提交)。[3.1]

Polzin, K.L.e . Kunze j . m . Toole和r·w·施密特,2000 b:小规模能量的分区内波和地转运动。期刊。Oceanogr。(提交)。[5.2]桥,r . M。,1994:Understanding the relation between wind- and pressure-driven sea-level variability. J. Geophys. Res. 99, 8033-8039. [3.3] Ponte, R. M. and P. Gaspar, 1999: Regional analysis of the inverted barometer effect over the global ocean using TOPEX/POSEIDON data and model results. J. Geophys. Res. 104, 1558715602. [3.3]

桥、智慧化和j . Luyten 1989:分析和解释在赤道太平洋赤道洋流。期刊。Oceanogr。19日,1025 - 1038。[4.3]

1990年桥,r . m . j . Luyten:深速度测量在西印度洋赤道。期刊。44-52 Oceanogr。20日。[4.3]桥,r . M。,J。R. Luyten and P. L. Richardson, 1990: Equatorial deep jets in the Atlantic Ocean. Deep-Sea Res. 37, 711-713. [4.5, 5.2] Potemra, J., 1999: Seasonal variations of upper ocean transport from the Pacific to the Indian Ocean via Indonesian Straits. J. Phys. Oceanogr. 29, 2930-2944. [4.7] Potemra, J.T., R. Lukas and G.T. Mitchum, 1997: Large-scale estimation of transport from the Pacific to the Indian Ocean. J. Geophys. Res. 102, 27795-27812. [3.3, 4.7] Poulain, P.-M., 1993: Estimates of horizontal divergence and vertical velocity in the Equatorial Pacific. J. Phys. Oceanogr. 23, 601-607. [4.1]

也不会。下午。P.P. Niiler, 1989:统计分析表面循环在加利福尼亚海流系统使用satellite-tracked流浪者。期刊。Oceanogr。19日,1588 - 1601。[4.1]也不会,下午。,J。D. Illeman and P. P. Niiler, 1987: Drifter observations in the California Current System 1985-1986.斯克里普斯海洋研究所的加州大学,圣地亚哥。数据报告、SIO Ref。87 - 27, 72页。[4.1]

也不会,下午。a . Warn-Varnas和p p . Niiler 1996:北欧海的近地表循环以拉格朗日漂流者。j .地球物理学。研究》101年,18237 - 18258。[4.1]普拉特,剩下P.A. Lundberg, 1991:液压旋转海峡和窗台上的流。安。启流体机械。23日,81 - 106。[5.6]普伦蒂斯,智能卡g·法夸尔,m . Fasham et al ., 2001:碳循环和大气中的二氧化碳。:政府间气候变化专门委员会工作小组1,第三次评估报告,剑桥大学出版社,第三章[1.2]价格,参考书籍和m . o .霸菱1994:外流和深水生产边际的海洋。 Prog. Oceanogr. 33, 161-200. [2.2, 5.2] Price, J.F. and J. Yang, 1998: Marginal sea overflows for climate simulations. In:海洋建模和参数化,e . p . Chassignet和j . Verron (eds),提供专科学校出版。多德雷赫特,155 - 170页。[5.2]

价格,j·F。,r·a·韦勒和r . Pinkel 1986:昼夜循环:海洋观测和模型上对日加热、冷却、混合和风力。j .地球物理学。研究》91年,8411 - 8427。[7.2]

价格,j·F。,r·a·韦勒和水银血压计Schudlich, 1987:风动洋流和埃克曼输送。科学23,1534 - 1538。[4.1]价格,j·F。m . o .霸菱,r . g . Lueck et al ., 1993:地中海流出混合和动力学。259年科学,1277 - 1282。[5.2]教务长,C。a, c·艾斯可菲,k . Maamaatuaiahutapu Kartavtseef诉男孩,1999:亚热带模式在南大西洋水域。j .地球物理学。研究》104年,21033 - 21049。[5.4]秋B。, 1992: Recirculation and seasonal change of the Kuroshio from altimetry observations. J. Geophys. Res. 97, 17801-17813. [3.3] Qiu, B., 1994: Determining the mean Gulf Stream and its recirculations through combining hydro-graphic and altimetric data. J. Geophys. Res. 99, 951-962. [3.3] Qiu, B., 1995: Variability and energetics of the Kuroshio Extension and its recirculation gyre from the first two-year TOPEX data. J. Phys. Oceanogr. 25, 1827-1842. [3.3] Qiu, B., 1999: Seasonal eddy field modulation of the North Pacific subtropical Countercurrent: TOPEX/ POSEIDON observations and theory. J. Phys. Oceanogr. 29, 2471-2486. [3.3] Qiu, B. and F.-F. Jin, 1997: Antarctic circumpolar wave: an indication of ocean-atmosphere coupling in the extratropics. Geophys. Res. Lett. 24, 2585-2588. [4.6] Qiu, B. and T. M. Joyce, 1992: Interannual variability in the mid- and low-latitude western North

太平洋。期刊。Oceanogr。22日,1062 - 1079。[7.3,7.4]

1993年秋b和k·a·凯利:上层海洋黑潮延伸地区的热平衡。期刊。Oceanogr。23日,2027 - 2041。邱[3.3]。B。k·a·凯利和T.M.乔伊斯,1991:平均流量和可变性黑潮延伸从地质卫星测高数据。j .地球物理学。研究》96年,18491 - 18507。[3.3]秋B。,苗w·p·穆勒,1997:强迫和自由斜压罗斯比波的传播和衰减在off-equatorial海洋。期刊。 Oceanogr. 27, 2405-2417. [3.3] Quadfasel, D. and F. Schott, 1982: Water mass distribution at intermediate layers off the Somali coast during the onset of the西南季风,1979年。期刊。Oceanogr。1358 - 1372。[4.3]Quadfasel、d和f . Schott 1983:向南地下流以下索马里当前。j .地球物理学。研究》88年,5973 - 5979。[4.3]Quadfasel D。a . Sy, d井和a . Tunik 1991:

在北极变暖。大自然350年,385年。[7.3]Quadfasel D。a . Frische和g . Cresswell 1996:循环的源区南赤道海流在东印度洋。j .地球物理学。研究》101年,12483 - 12488。[4.7]Quadfasel D。,J。Fischer, F. Schott and L. Stramma, 1997: Deep water exchange through the Owen断裂带在阿拉伯海。地球物理学。卷。24日,2805 - 2808。[4.3]码头,警察局,至此,m . Stuiver和布勒克1983:赤道太平洋上升流率来自14 c分布。769 - 792 j . 3月41号决议。[4.4]Quilfen, Y。B。Chapron, T. Elfouhaily, K. B. Katsaros and J. Tournadre, 1998: Observations of tropical cyclones by high-resolution scatterometry. J. Geophys. Res. 103, 7767-7786. [3.4] Rahmstorf, S., 1995:分支,大西洋温盐环流的变化而在水文循环。大自然378年,145 - 149。[4.7,7.2]拉姆斯托夫,S。1996:淡水强迫和北大西洋温盐环流的运输。raybet雷竞技最新气候动力学。799 - 811。(2.3,4.7,6.2)拉姆斯托夫,S。2001:突然的气候变化。raybet雷竞技最新:海洋科学百科全书的j·斯蒂尔,索普和k Turekian (eds),学术出版社,伦敦。[1.2]拉姆斯托夫,s和a . Ganopolski 1999:长期全球变暖情况计算与一个高效耦合气候模式。raybet雷竞技最新气候变化,43岁,353 - 367。 [1.1, 1.2, 2.3, 7.3] Rahmstorf, S. and J. Willebrand, 1995: The role of temperature feedback in stabilising the thermohaline circulation. J. Phys. Oceanogr. 25, 787-805. [1.1, 2.3, 7.2]

拉姆斯托夫,S。,J。Marotzke and J. Willebrand, 1996: Stability of the thermohaline circulation. In: The Warmwatersphere of the North Atlantic Ocean, W. Krauss (ed.), Gebr. Bornträger, Stuttgart, pp. 129-157. [2.3, 7.2] Ralph, E.A. and P.P. Niiler, 1999: Wind-driven currents in the tropical Pacific. J. Phys. Oceanogr. 29, 2121-2129. [4.1, 7.1] Ralph, E., K. Bi, P. Niiler and Y. duPenhoat, 1997: A Lagrangian description of the western equatorial Pacific response to the wind burst of December 1992: Heat advection of the Warm Pool. J. Climate 10, 1706-1721. [4.1] Raney, R.K., 1998: The delay/Doppler radar altimeter. IEEE Trans. Geoscience Remote Sens. 36, 1578-1588. [3.3] Rao, R. R. and R. Sivakumar, 2000: On the possible mechanisms of the evolution of a mini-Warm Pool during the pre-summer雨季和创世纪东南部出现漩涡的阿拉伯海。夸脱。j·罗伊。流星。Soc。(印刷中)。[4.3]

饶,水银血压计R.L.莫伦纳和参考书籍祭日,1989:进化的气候热带印度洋的近地表热结构我:每月的描述混合层深度,海洋表面温度,表面流和地面气象领域。j .地球物理学。94号决议1080110815。[4.3]

拉普,r·h·y·m·王,1994:动态地形估计使用地质卫星数据和在墨西哥湾流地区重力大地水准面。地球物理学。j . Int。117年,511 - 528。[3.3]拉普,相对湿度,张和y, 1996:动态使用TOPEX海洋地形数据的分析和正交函数。j .地球物理学。研究》101年,22583 - 22598。[3.3]Ratier, a(主编),1988:观察测高法的海洋。研究杂志,3号,1998年10月。中心国家d作为,图卢兹(http://www.cnes.fr/WEB_UK/espace_pro/cnesmag/lindex.html), 11-29页。[1.3]雷纳,附加说明福兰德,E.B.霍顿,D.E.帕克,C.K.哈克特R.B., 1996: 2.2版本的全球海冰与海洋表面温度数据集,1903 - 1994。哈德利中心CRTN 74年,英国气象办公室,布拉克内尔,。[2.3]阅读、参考书籍和j•古尔德,1992:冷却和淡化的近极的北大西洋自1960年代。360年自然,55-57。[1.2,7.3]阅读、参考书籍和保留时间波拉德,1993:南极绕极流的结构和运输Agulhas返回当前在40°E。j .地球物理学。研究》98年,12281 - 12295。[4.6,4.7]阅读、参考书籍和保留时间波拉德,1997:深流入到莫桑比克盆地。国际WOCE

通迅,29号7 - 10,WOCE国际项目办公室(未发表的文件)。[4.5]收获颇丰,r和漫画去骨,1997:效应溢出的近极的北大西洋环流;一个区域模型研究。j .地球物理学。研究》102年,18529 - 18552。[2.2,2.3]收获颇丰,r . j . Dengg 1999:传播的氟里昂不同分辨率的数值模型。国际WOCE通讯,35号,12 - 14,WOCE国际项目办公室。(未发表的文件)。[2.2]里德,评论1965年:中间的太平洋水域。约翰霍普金斯海洋研究,85页。[4.4,5.4]里德,j·L。1978:中深循环在北大西洋和盐度场。 J. Geophys. Res. 83, 5063-5067. [5.7] Reid, J.L., 1979: On the contribution of the Mediterranean Sea outflow to the Norwegian-Greenland Sea. Deep-Sea Res. 26, 1199-1223. [5.7]

•里德。1981:在世界中深循环的海洋。:物理海洋学的进化,b . a·沃伦和c·温斯迟(eds),麻省理工学院出版社,剑桥,妈,70 - 111。雷竞技csgo[4.2]里德,评论1982:在使用冬季对流的溶解氧浓度作为指标。海军启34号决议28-39。[5.4]里德,评论1986:总数循环地转南太平洋的流动模式、路径和传输。掠夺。Oceanogr。16日,1 - 61。[4.2,4.4]里德,评论1989:在南大西洋的总地转循环:流模式、路径和传输。掠夺。Oceanogr。23日,149 - 244。[4.2,4.5]里德,评论,1994:On the total geostrophic circulation of the North Atlantic Ocean: Flow patterns, tracers, and transports. Prog. Oceanogr. 33, 1-92. [4.2, 5.7, 7.1] Reid, J.L., 1997: On the total geostrophic circulation of the Pacific Ocean: flow patterns, tracers and transports. Prog. Oceanogr. 39, 263-352. [3.2, 4.2, 4.7, 5.8, 7.1] Reid, J. and A. Mantyla, 1995: World dataset, ftp site minerva ucsd.edu, San Diego. [7.3] Reid, Jr., J.L. and R.J. Lynn, 1971: On the influence of the Norwegian-Greenland and Weddell seas upon the bottom waters of the Indian and Pacific Oceans. Deep-Sea Res. 18, 1063-1088. [4.6] Reid, Jr., J.L., and W.D. Nowlin, Jr., 1971: Transport of water through Drake Passage. Deep-Sea Res. 18, 51-64. [4.6] Reid, Jr., J.L., W.D. Nowlin, Jr. and W.C. Patzert, 1977: On the characteristics and circulation of the southwestern Atlantic Ocean. J. Phys. Oceanogr. 7, 62-91. [4.6]

瑞德,B。Planque and M. Edwards, 1998: Is observed variability in the long-term results of the Continuous Plankton Recorder survey a response to climate change? Fisheries Oceanography 7, 282-288. [1.2] Reppin, J., F. A. Schott and J. Fischer, 1999: Equatorial currents and transports in the upper central Indian Ocean: Annual cycle and inter-annual variability. J. Geophys. Res. 104, 1549515514. [4.3]

Reverdin G。1987:上赤道印度洋:气候季节性周期。期刊。Oceanogr。903 - 927。[4.3]Reverdin G。,农村,y du Penhoat y Gouriou, 1991:垂直结构的季节性周期在中央赤道大西洋:XBT部分准确性从1980年到1988年。期刊。Oceanogr。21日,277 - 291。[4.3]Reverdin G。c . Frankignoul,大肠Kestenare和m . j . McPhaden 1994:季节性变化在赤道太平洋的表面电流。 J. Geophys. Res. 99, 20323-20344. [4.1, 4.3] Reynolds, R.R. and T.M. Smith, 1994: Improved global sea surface temperature analyses using optimum interpolation. J. Climate 7, 929-948. [3.4, 4.1, 5.1, 7.1]

大黄酸,M。,1994:The Deep Western Boundary Current: Tracers and velocities, Deep-Sea Res. 41, 263-281. [5.8] Rhein, M., L. Stramma and U. Send, 1995: The Atlantic Deep Western Boundary Current: Water masses and transports near the equator. J. Geophys. Res. 100, 2441-2457. [4.3, 4.5, 5.8]

大黄酸,M。l . Stramma g . Krahmann, 1998:热带大西洋南极底层水的扩散。深海> 45岁,507 - 527。[4.6,5.8]

大黄酸,M。o . Plahn r .拜耳,l . Stramma m·阿诺德,1998 b:示踪剂的演化电流信号在深的西部边界,热带大西洋。j .地球物理学研究》103年,15869 - 15883。[5.8]大黄酸,M。,J。Fischer, W.M. Smethie et al., 2001: Labrador Sea Water: Pathways, CFC-inventory and formation rates. J. Phys. Oceanogr. (In press)663. [5.8] Rhines, P. B., 1994: Climate change in the Labrador Sea, its convection and circulation. In: Atlantic Climate Change Program, Proceedings of the Principal Investigators' Meeting, Princeton, NJ, 911 May 1994, pp. 85-96. [7.3] Rhines, P.B., 1998: Circulation, convection and mixing in rotating, stratified basins with sloping topography. In: Physical Processes in Lakes and Oceans, J. Imberger (ed.), American Geophysical

联盟,华盛顿特区、沿海和河口系列,54卷,第435 - 451页。[5.5]莱茵河,回堵1993:海洋环流:波和海面动力学。造型:海洋交互,j . Willebrand和安德森(eds),北约麻生太郎系列,施普林格,柏林,页67 - 149。[5.1]莱茵河,P.B.和得到年轻,1982:风力驱动循环的理论。j . 3月> 559596。[4.2]

莱茵河,P.B.和得到年轻,1982 b: Homog-enization潜在行星旋转的涡度。j .流体机械。122年,347 - 367。[4.2]Ribbe, J。1997:是什么驱使中期纬度对流和亚南极的模式的形成水。国际WOCE通讯,29号,20到25日至26日,WOCE国际项目办公室(未发表的文件)。[5.4]Ribbe, j . m . Tomczak 1997:失踪的印尼通流的影响在南极高分辨率模型中,期刊。Oceanogr。27日,445 - 455。[4.7]Ribbe, j . m . Tomczak 1997 b:对流、俯冲和南极洲的形成模式南极Model-FRAM水在高分辨率。j . Sys。3月13日,137154年。[5.4]

理查兹,kj1998:在赤道交错:其参数化和大规模的影响。在海洋:建模和参数化,大肠Chassignet和j . Verron (eds),北约科学系列,系列C:数学。理论物理。科学。,Kluwer学会出版。多德雷赫特,235 - 252页。理查兹[4.3],k·j·r·波拉德,1991:上部结构的海洋在赤道太平洋西部。350年自然,48-50。理查森[4.3],p . L。, 1989: Worldwide ship drift distributions identify missing data. J. Geophys. Res. 96, 6169-6176. [4.1] Richardson, P. L., 1997: Drifting in the wind: leeway error in shipdrift data. Deep-Sea Res. I 44, 1877-1903. [4.1] Richardson, P. L. and D. M. Fratantoni, 1999: Float trajectories in the deep western boundary current and deep equatorial jets in the tropical Atlantic. Deep-Sea Res. II 46, 305-334. [4.3, 4.5] Richardson, P. L. and G. Reverdin, 1987: Seasonal cycle of velocity in the Atlantic North赤道逆流以表面流浪者,当前的米和船舶数据。j .地球物理学。研究》92年,3691 - 3708。[3.3]理查森,P.L.和j•施密茨,Jr .) 1993:越赤道气流深处与迄今为止,漂浮在大西洋测量。j .地球物理学。98号决议83718387。[4.3]

理查森,p . L。d·沃尔什,l . Armi m·施罗德和j . f .价格1989:跟踪三个美迪迄今为止,漂浮。期刊。Oceanogr。19日,371 - 383。[5.7]

理查森,p . L。A . s . Bower和w·泽克,2000:人口普查的美迪追踪的花车。掠夺。Oceanogr。45岁,209 - 250。[3.2]Rienecker, M . M。a . Borovikov, c . Keppenne和d . Adamec 1999:多元同化影响热带太平洋的状态的估计。:学报第三世界气象组织研讨会在气象学和海洋学数据同化,魁北克。[7.4]Rintoul,狭义相对论,1991:南大西洋流域间交换。j .地球物理学。 Res. 96, 2675-2692. [4.6, 4.7, 5.8, 6.1, 7.1] Rintoul, S. R., 1998: On the origin and influence of Adélie Land Bottom Water. In:海洋,冰和大气:交互在南极大陆边缘,南极研究系列的75卷,S.S.雅各布斯和r·维斯(eds),美国地球物理联盟,华盛顿特区,151171页。[4.6]

Rintoul, s . r . j . l . Bullister 1999:冬末水文部分从塔斯马尼亚到南极洲。深海研究》46岁,1417 - 1454。[4.6,4.7]

Rintoul r和s . sokolv, 2000:斜压运输可变性的南极绕极流南澳大利亚(WOCE重复部分SR3)。j .地球物理学。研究》(新闻)。[4.6]Rintoul,狭义相对论和c·温斯迟1991:质量,热、氧气和养分通量在北大西洋和预算。深海研究杂志38(增刊),S355-S377。[6.3]Rintoul,狭义相对论美国精英,J.A.教堂,2001:6年的记录南国的夏天斜压南极绕极流的交通变化在140°E,来自XBT和高度计测量准确性。j .地球物理学。研究》(提交)。[4.6]立管、南卡罗来纳州和t·罗斯比1983:Quasi-Lagrangian亚热带西部北大西洋环流的结构和变化。 J. Mar. Res. 41, 127-162. [3.2] Rix, N. and J. Willebrand, 1996: Parameterization of mesoscale eddies as inferred from a highresolution model. J. Phys. Oceanogr. 26, 2281-2285. [2.2] Roach, A.T., K. Aagaard, C.H. Pease et al., 1995: Direct measurements of transport and water properties through the Bering Strait. J. Geophys. Res. 100, 18443-18458. [4.7] Robbins, P. E., 2001: Oceanic carbon transport carried by freshwater divergence: are salinity normalizations useful? J. Geophys. Res. (submitted). [6.3]

罗宾斯,p . e . w·j·詹金斯,1998:tritium-3He年龄的观察时间的变化在北大西洋东部温跃层:证据改变通风?1125 - 1161 j . 3月56号决议。[5.3]罗宾斯,体育和J.M. Toole, 1997:溶解二氧化硅预算约束在印度洋的经向翻转环流。深海研究》44岁,879 - 906。(4.3,4.7,5.2,6.1,6.2)罗宾斯,体育,J。F. Price, W.B. Owens and W.J. Jenkins, 2000: On the importance of lateral diffusion for the ventilation of the lower thermocline in the subtropical North Atlantic. J. Phys. Oceanogr. 30, 67-89. [4.2, 5.3, 5.8] Roberts, M.J. and R. A. Wood, 1997: Topographic sensitivity studies with a Bryan-Cox-type ocean model. J. Phys. Oceanogr. 27, 823-836. [2.2, 2.3, 5.6]

罗伯茨,m . J。r·马什,a·l·r·a·伍德,1996:Bryan-Cox-type海洋模型和一个的相互比较等密度的海洋模型。第一部分:副极地环流和高纬度地区的过程。期刊。Oceanogr。26日,1495 - 1527。[2.2,2.3]Robertson a W。1996年:在北太平洋年代际变化multi-century气候模拟。raybet雷竞技最新raybet雷竞技最新气候动力学。227 - 241。[2.3]罗宾逊,a . r .(主编),1983:在海洋漩涡

科学。斯普林格出版社,海德堡609页。[1.3]罗宾逊,a·r·h·Stommel, 1959:海洋温跃层和温盐环流有关。忒勒斯11日295 - 308。[4.4]罗宾逊,a . r和p . Welander 1963:热循环旋转球体:海洋温跃层与应用程序。25-38 j .研究》3月21日。[4.4]

罗宾逊,a。R。d·e·哈里森,y明茨和a·j·Semtner 1977:漩涡和一种理想化的环流海洋环流:风和热驱动原始方程数值实验。期刊。Oceanogr。7, 182 - 207。[2.2]Robitaille,共晶和A.J.韦弗,1995:验证subgrid-scale混合方案使用氯氟烃在全球海洋模型。地球物理学。卷。22日,2917 - 2920。[2.3]登,特种部队,1970:太平洋的过渡区。j .地球物理学。研究》75年,1097 - 1109。 [5.4] Roden, G.I., 1998: Upper海洋温跃层、氧气、营养和流动结构附近的日期在1993年的夏天。j .地球物理学。研究》103年,12919 - 12939。[4.3]罗德里格斯,E。B。Pollard and J. Martin, 2000: Wide swathe ocean altimetry using雷达干涉测量。IEEE反式。,Geosci。远程参议员(新闻)。[3.3]-罗德维尔,M.J.福兰德D.P.罗和C.K., 1999:冬季北大西洋海洋强迫

振荡和欧洲的气候。raybet雷竞技最新大自然398年,320 - 323。[1.2,2.3]Roeckner E。,J。M. Oberhuber, A. Bacher, M. Christoph and I. Kirchner, 1996: ENSO variability and atmospheric response in a global coupled atmosphere-ocean GCM. Climate Dyn. 12, 737-754. [2.3] Roemmich, D., 1983: The balance of geostrophic and Ekman transports in the equatorial Atlantic Ocean. J. Phys. Oceanogr. 13, 1534-1539. [4.3] Roemmich, D., 1987: Estimates of net transport, upwelling, and heat flux in the tropical oceans from inverse methods and related geostrophic methods. In: Further Progress in Equatorial Oceanography, E. Katz and J. Witte (eds), Nova University Press, pp. 165-176. [4.4] Roemmich, D. and B. Cornuelle, 1992: The Subtropical Mode Water of the South Pacific Ocean. J. Phys. Oceanogr. 22, 1178-1187. [5.4] Roemmich, D. and B. Cornuelle, 1993: How representative are individual hydrographic sections of the long-term behaviour of the oceans? In: Workshop on the Use of Sub-Surface Thermal Data for Climate Studies, Brest, France, 13-16 September 1993, Int. TOGA Project Office, Report No. 9/WOCE Report No. 110/93, 64 pp. [7.4] Roemmich, D. and J. Gilson, 2000: Eddy transport of heat and thermocline waters in the North Pacific: A key to interannual/decadal climate variability? J. Phys. Oceanogr. (in press). [7.4] Roemmich, D. and T. McCallister, 1989: Large scale circulation of the North Pacific Ocean. Prog. Oceanogr. 22, 171-204. [4.5, 5.2, 6.1, 6.2] Roemmich, D. and C. Wunsch, 1984: Apparent changes in the climatic state of the deep North Atlantic Ocean. Nature 307, 447-450. [7.3] Roemmich, D. and C. Wunsch, 1985: Two transatlantic sections: meridional circulation and heat flux in the subtropical North Atlantic Ocean. Deep-Sea Res. 32, 619-664. [2.2, 6.3] Roemmich, D., S. Hautala and D. Rudnick, 1996: Northward abyssal transport through the Samoan Passage and adjacent regions. J. Geophys. Res. 101, 14039-14055. [4.5, 5.2] Roemmich, D., J. Gilson, B. Cornuelle and R. Weller, 2000: The mean and time-varying meridional transport of heat at the tropical/subtropical boundary of the North Pacific Ocean. J. Geophys. Res. (submitted). [7.1] Roether, W. and A. Putzka, 1996: Transient-tracer information on ventilation and transport of South Atlantic Waters. In: The South Atlantic: Present and Past Circulation, G. Wefer, W. H. Berger, G. Siedler and D.J. Webb (eds), Springer-Verlag, Berlin, pp. 45-62. [5.8, 6.3]

Roether, w . m .大黄酸,1989:海洋化学示踪剂。新系列:Landolt-Bornstein, V, 3 b卷,j . Sundermann(主编),SpringerVerlag, 4.3章,页59 - 122。[5.8]Roether, W。B。Manca, B. Klein et al., 1996: Recent Changes in the Eastern Mediterranean Deep Waters. Science 271, 333-335. [5.7] Rogers, J.C., 1990: Patterns of low-frequency monthly海平面压力变化(1899 - 1986)和相关波风暴频率。j .raybet雷竞技最新气候3,1364 - 1379。[7.3]罗杰斯J.C.,1994:Atlantic storm track variability and the North Atlantic Oscillation. In: Atlantic Climate Change Program: Proceedings of the Principal Investigators' Meeting, Princeton, NJ, 9-11 May 1994, pp. 20-24. [7.3] Rogers, J.C., 1997: North Atlantic storm track variability and its association to the North Atlantic Oscillation and climate variability of Northern Europe. J. Climate 10, 1635-1647. [7.3] Rogers, J. C. and H. van Loon, 1982: Spatial variability of sea level pressure and 500 mb height anomalies over the Southern Hemisphere. Mon. Wea. Rev. 110, 1375-1392. [7.3] Rohling, E.J. and H.L. Bryden, 1992: Man-induced盐度和温度增加西部地中海深水。j .地球物理学。研究》97年,11雷竞技csgo191 - 11198。[5.7]Rooth C.G.和H.G. Ostlund, 1972:氚渗透到大西洋温跃层。深海研究》19日481 - 492。[5.8]Ropelewski, c·f·p·d·琼斯,1987:Tahiti-Darwin南方涛动指数的延伸。星期一,我们。115年启,2161 - 2165。[7.1]Rosati, A和k . Miyakoda 1988:对上层海洋环流模式模拟。期刊。 Oceanogr. 18, 1601-1626. [5.1] Rose, H., 1999: Untersuchung der Zirkulation und der Erneuerung des Antarktischen Zwischenwassers im Südatlantic aus FCKW-Daten, Doctoral Dissertation, University of Bremen, Sept. 1999, 148 pp. [5.8] Rosen, R. D., 1999: The global energy cycle. In: Global Energy and水的循环k·a·布朗宁和r . j .格尼(eds),剑桥大学出版社,292页。[6.2]Roson, G。自动跟踪,里奥斯,拉文,F.F.佩雷斯和上半叶。布莱登指出,他2001:碳分布、通量和预算在亚热带北大西洋(24.5°N)。j .地球物理学。研究》(提交)。[6.3]

罗斯,c。,1976:73 -运输溢出的水溢出通过丹麦海峡。国际海洋勘探理事会,哥本哈根。冰厘米1976 / C: 15。[5.6]

罗斯比,c·G。,1936:稳定的洋流的动力学实验流体力学。论文在物理海洋学和气象学、5、1。[7.4]

罗斯比,c·G。1937:相互调整的压力和速度分布在某些简单的当前系统。j . 3月1号决议15-28。[7.4]罗斯比,热处理1983年,南卡罗莱纳州立管和A.J. Mariano:北大西洋西部——拉格朗日观点。在海洋科学:涡流,a·r·罗宾逊(主编),斯普林格出版社,柏林,页66 - 91。[3.2]

罗斯比,h·T。e·r·莱文和d·n·康纳斯,1985:等密度的吞下浮动-一个简单的装置跟踪水包裹在海洋里。掠夺。Oceanogr。511 - 525。[3.2]罗斯比,T。1996年:北方大西洋海流和周围的水域中:在十字路口。启“。34岁,463 - 481。[3.2,7.1]罗斯比,t·e·戈特利布,1998:夹竹桃项目:监控墨西哥湾流的可变性和附近海域在新泽西和百慕大群岛之间。公牛。阿米尔。流星。Soc。79年,5日至18日期间召开。[1.2,3.1]

罗斯比、t和d·韦伯,1970:观察到深海运动通过跟踪吞下漂浮在通道。深海研究》17,359 - 365。[3.2]罗斯比,T。d . Dorson和j·方丹,1986:批系统。j .大气压。海洋抛光工艺。672 - 679。[3.2]罗斯比,T。小时m.d.多嘴的人。Zhang et al . 2000:温水近极的北大西洋的途径:一些案例研究。38号,17日至19日国际WOCE通讯WOCE国际项目办公室(未发表的文件)。 [3.2] Rossow, W.B. and R. A. Schiffer, 1991: ISCCP cloud data products. Bull. Amer. Meteor. Soc. 72, 2-20. [3.4, 5.1]

Rothstein L.M.,M.J. McPhaden P.A. Proehl, 1988:风强迫wave-mean流相互作用在赤道波导。第一部分:开尔文波。期刊。Oceanogr。18日,1435 - 1447。[4.3]Rothstein, l . M。张,r·h·A·j·Busalacchi d·陈,1988 b:数值模拟的意思是水通道的亚热带和热带太平洋。期刊。Oceanogr。28岁,322 - 342。[4.4]Roullet, g, g . Madec 2000:盐保护,自由表面和不同层次:海洋模型的新配方。j .地球物理学。研究》105年,23927 - 23942。 [2.3] Rowe, G. D., E. Firing and G. C. Johnson, 2000: Pacific equatorial subsurface countercurrent velocity, transport, and potential vorticity. J. Phys. Oceanogr. 30, 1172-1187. [3.1, 4.3]

鲁迪,b和d·赫伯特,1988:美迪沙龙的混合。:小规模动荡和混合在海洋中,J.C.J. Nihoul和B.M. Jamart (eds),爱思唯尔科学出版。,249 - 261页。[5.2]鲁迪,B。d·沃尔什和n .太走运,1997:明显的变化在北大西洋中部水混合效率。期刊。Oceanogr。27日,2589 - 2605。[5.2]Rudels, B。,1995:The thermohaline circulation of the Arctic Ocean and the Greenland Sea. Phil. Trans. Roy. Soc. Lond. A 352, 287-299. [7.3] Rudels, B. and D. Quadfasel, 1991: Convection and deep water formation in the Arctic Ocean-Greenland Sea system. J. Mar. Sys. 2(3/4), 435450. [1.2, 7.3] Rudels, B., D. Quadfasel, H. Friedrich and M.-N. Houssais, 1989: Greenland Sea convection in the winter of 1987-1988. J. Geophys. Res. 94, 3223-3227. [1.2] Rudels, B., E. Jones, L. Anderson and G. Kattner, 1994: On the intermediate depth waters of the Arctic Ocean. In: The Polar Oceans and their Role in Shaping the Global Environment, O. M. Johannessen, R. D. Muench and J. E. Overland (eds), American Geophysical Union, Washington, DC, pp. 5-20. [4.7] Rudels, B., L. Anderson and E. Jones, 1996: Formation and evolution of the surface mixed layer and halocline of the Arctic Ocean. J. Geophys. Res. 101, 8807-8821. [4.7] Rudnick, D.L., 1997: Direct velocity measurements in the Samoan Passage. J. Geophys. Res., 102, 3293-3302. [4.5] Rudnick, D. L. and R. Ferrari, 1999: Compensation of horizontal temperature and salinity gradients in the海洋混合层。283年科学,526 - 529。[5.2,5.5]拉姆福德,B。1800年,计数:第七篇,在液体热量的传播。:散文,政治、经济、和窥探影影绰绰,一个新的版本,t·卡德尔jr .)和w·戴维斯(eds),伦敦,197 - 386页。[4.4]露丝,C。,r . w . Roether, 2000:原始3他在南大西洋深海大洋中脊来源。深海研究》1059 - 1075页。[4.5]Sabine,中一段和m .钥匙,1997:地表水和大气进行碳期间获取的数据世界海洋环流实验印度洋调查邮轮(R / V家乐,1994年12月- 1996年1月)。二氧化碳信息分析中心,橡树岭国家实验室,美国能源部橡树岭,TN,美国ORNL /人均排放- 103,民主党- 064、38页。[6.3]

Sabine,中一段,D.W.R.华莱士和F.J. Millero, 1997:海洋中二氧化碳的调查揭示对全球碳循环的线索。Eos反式。阿米尔。地球物理学。联盟。78年,54-55。[6.3]Sabine,中一段智慧化关键K.M. Johnson et al ., 1999:人为二氧化碳的印度洋库存。水珠。Biogeochem。 Cycles, 13,179-198. [6.3] Saji, N. H., B. N. Goswami, P. N. Vinayachandran and T. Yamagata, 1999: A dipole mode in the tropical Indian Ocean. Nature 401, 360-363. [1.2, 4.3, 7.1] Salmon, R., 1999: The lattice Boltzmann method as a basis for ocean circulation modeling. J. Mar. Res. 57, 503-535. [7.2] Salmon, R. and R. Hollerbach, 1991: Similarity solutions of the thermocline equations. J. Mar. Res. 49, 249-280. [2.2] Samelson, R. M., 1998: Large-scale circulation with locally enhanced vertical mixing. J. Phys. Oceanogr. 28, 712-726. [4.2] Sandström, J.W., 1916: Meteorologische Studien im schwedischen Hochgebirge. Goteborgs K. Ventenskaps-och Vitterhetssamhalles Handl, Series 4, 22(2), 48 pp. [5.2] Sandström, J.W. and B. Helland-Hansen, 1903: Über die Berechnung von Meereströmungen. Reports on Norwegian Fishery and Marine Investigations, Bergen, Vol. 2(4), 43 pp. [3.2] Saravanan, R., 1998: Atmospheric low-frequency variability and its relationship to midlatitude SST variability: studies using the NCAR Climate System Model. J. Climate 11, 1386-1404. [2.3] Saravanan, R., G. Danabasoglu, S. C. Doney and J. C. McWilliams, 2000: Decadal variability and predictability in the midlatitude ocean-atmosphere system. J. Climate 13, 1073-1097. [2.3] Sarmiento, J. L., 1983: A tritium box model of the North Atlantic thermocline. J. Phys. Oceanogr. 13, 1269-1274. [5.3, 5.4] Sarmiento, J. L., 1986: On The North and Tropical Atlantic heat balance. J. Geophys. Res. 91, 641-657. [2.2] Sarmiento, J. L. and E. T. Sundquist, 1992: Revised budget for the oceanic uptake of anthropogenic carbon-dioxide. Nature 356, 589-593. [6.3] Sarmiento, J.L., C. G.H. Rooth and W. Roether, 1982: The North Atlantic tritium distribution in 1972. J. Geophys. Res. 87, 8047-8056. [4.4, 5.4]

Sarmiento J.L.,J。C. Orr and U. Siegenthaler, 1992: A perturbation simulation of CO2 uptake in an ocean general circulation model. J. Geophys. Res. 97, 3621-3636. [6.3] Sarmiento, J.L., R. Murnane and C. le Quéré, 1995: Air-sea CO2 transfer and the carbon budget of the

北大西洋,菲尔。反式。罗伊。Soc。Lond。348年,211 - 219。[6.3]Sarmiento J.L.,R.J.史托福和美国Manabe T.M.C.休斯1998:刺激响应的海洋碳循环人为气候变暖。raybet雷竞技最新大自然393年,245 - 249。佐藤[1.1,1.2],职能, P.S. Polito and W.T. Liu, 2000: Importance of salinity measurements in the heat storage estimation from TOPEX/POSEIDON. Geophys. Res. Lett. 27, 549-551. [3.3] Saunders, P.M., 1987: Flow through Discovery Gap.

期刊。Oceanogr。631 - 643。桑德斯(4.5,5.2,5.6),p . M。从法罗银行,1990:冷流出渠道。期刊。29-43 Oceanogr。20日。[5.6]

桑德斯,点,1994:The flux of overflow water through the Charlie-Gibbs Fracture Zone. J. Geophys. Res. 99, 12343-12355. [4.5, 5.6] Saunders, P. M., 1996: The flux of dense cold water overflow southeast of Iceland. J. Phys. Oceanogr. 26, 85-95. [4.5, 5.6] Saunders, P.M. and W.J. Gould, 1988: CTD data from RRS Challenger cruise 15/87 around the Faroe Islands. Inst. Oceanogr. Sci., Deacon Lab., Report No. 256, 79 pp. [5.6] Saunders, P. M. and B. A. King, 1995a:底流来自一个船载ADCP WOCE巡航A11在南大西洋。期刊。Oceanogr。25日,329 - 347。[3.1]桑德斯,下午和文学士学位国王,1995 b:海洋通量WOCE A11部分。期刊。Oceanogr。25日,1942 - 1958。(2.3,3.1,4.2,4.6,4.7,6.1,6.2)

桑德斯,p . M。a . c .懦夫和b a de Cuevas 1999:太平洋的循环在全球海洋模型:海洋环流和气候raybet雷竞技最新先进的建模项目(奥卡姆)。j .地球物理学。研究》104年,18281 - 18299。(2.2,4.1,6.1)Sausen, R。k . Barthel k . Hasselmann, 1988:耦合的海洋大气模型通量校正。raybet雷竞技最新气候动力学。2,145 - 163。[2.3]席勒,。,1995:The mean circulation north of 30°S determined with the伴随方法应用到一个海洋环流模式。453 - 497 j . 3月53号决议。[7.2]席勒,。,J。S. Godfrey, P. C. McIntosh, G. Meyers and S.E. Wijffels, 1998: Seasonal near-surface dynamics and thermodynamics of the Indian Ocean and Indonesian Throughflow in a global ocean general circulation model. J. Phys. Oceanogr. 28, 2288-2312. [4.7] Schimel, D., D. Alves, I. Enting et al., 1996: CO2 and the carbon cycle. In: Climate Change 1995: The Science of Climate Change: Contribution of WG I to the Second Assessment Report of the IPCC,

j·t·霍顿et al . (eds),剑桥大学出版社,剑桥,页65 - 86。[6.3]施莱辛格,主机,柔若盖茨和Y.J.汉,1985:海洋CO2-induced气候变暖的作用:从俄勒冈州立大学耦合GCM硕士的初步结果。raybet雷竞技最新:海气耦合模式,J.C.J. Nihoul(主编),爱思唯尔,页447 - 478。[2.2]啤酒,R。,1995:An adjoint model for the determination of the mean oceanic circulation, air-sea fluxes and mixing coefficients. Berichte zur Polarforschung 156, 103 pp. [7.1] Schlitzer, R., 1996: Mass and heat transports in the South Atlantic derived from historical hydro-graphic data. In: The South Atlantic: Present and Past Circulation, G. Wefer, W. H. Berger, G. Siedler and D.J. Webb (eds), Springer-Verlag, Berlin, pp. 305-323. [4.7] Schlosser, P., 1986: Helium: a new tracer in Antarctic oceanography. Nature 321, 233-235. [5.8] Schlosser, P. and W.M. Smethie, Jr., 1995: Transient tracers as a tool to study variability of ocean circulation. In:自然气候变化raybet雷竞技最新Decade-to-Century时间尺度上,d·g·马丁森et al。(eds),国家研究委员会,国家科学院出版社,华盛顿特区,274 - 288页。[5.8]

施洛塞尔P。r .拜耳,a . Foldvik t . Gammelsred Rohardt和快速出拳Munnich, 1990: 18 o和氦作为示踪剂的冰架水和水/冰在威德尔海相互作用。j .地球物理学。研究》95年,3253 - 3263。[5.8],P。g . Bonisch, m .大黄酸和r .拜耳1991:减少在格陵兰海深水形成在1980年代:从示踪数据证据。251年科学,1054 - 1056。[7.3],P。,J。L. Bullister and R. Bayer, 1991b: Studies of deep water formation and circulation in the Weddell Sea using natural and anthropogenic tracers. Mar. Chem. 35, 97-122. [5.8] Schlosser, P., G. Bönisch, B. Kromer et al., 1995: Mid 1980s distribution of tritium, 3He, 14C and 39Ar in the Greenland/Norwegian seas and the Nansen Basin of the Arctic Ocean. Prog. Oceanogr. 35, 1-28. [5.8] Schmid, C., G. Siedler and W. Zenk, 2000: Dynamics of intermediate水循环在亚热带南大西洋。期刊。Oceanogr。3191 - 3211。[5.3]

施密特前作空。,1981:形式的温度盐度关系在中央水:double-diffusive混合的证据。期刊。Oceanogr。11日,1015 - 1026。[5.2]施密特,公债1988:混合在温盐楼梯。海洋中:小规模的动荡和混合,J.C.J. Nihoul和B.M. Jamart (eds),爱思唯尔,纽约,435 - 452页。[5.2]施密特,公债,1994:双扩散在海洋学。安。启流体机械。26日,255 - 286。[5.2]施密特,公债在海洋,1998:Double-diffusive对流:其作用混合大规模建模和参数化方案。在海洋:建模和参数化,大肠Chassignet和j . Verron (eds),提供专科学校出版。多德雷赫特,215 - 234页。[5.2]施密特,r·W。,1999:香料和妖精。科学

283年,498 - 499。[5.2]施密特,r·W。p s Bogden和c·e·多尔曼,1989:-降水和蒸发通量密度的北大西洋。期刊。Oceanogr。19日,1208 - 1221。[5.1]设a和t·f·斯托克1999:在全球变暖温盐环流的稳定性实验。j .raybet雷竞技最新气雷竞技csgo候12,1117 - 1133。j•施密茨[2.3]1988:探索涡流场的中纬度北太平洋。期刊。 Oceanogr. 18, 459-468. [3.2] Schmitz, W.J., 1995: On the interbasin-scale thermohaline circulation. Rev. Geophys, 33, 151-173. [4.2, 4.6, 4.7, 5.4, 7.1] Schmitz, W.J., 1996a: On the World Ocean Circulation. Vol. I: Some Global Features/North Atlantic Circulation.伍兹霍尔海洋机构,技术报告,whoi - 96 - 03、141页。施密茨(1.2,4.2,4.6,4.7),j1996 b:世界海洋环流,第二卷:太平洋和印度洋/全局更新。伍兹霍尔Oceano-graphic研究所、技术报告、whoi - 96 - 08年,237页。施密茨(1.2,4.2,4.6,4.7),j•理查森P.L., 1991:佛罗里达海流的来源。深海研究杂志38(增刊),S389-S409。施密茨[4.3],j和硕士麦卡特尼,1993:北大西洋环流。29-49启“。31日。施耐德(2.1,4.2,4.4,4.5),N。,1998:印尼直流和全球气候系统。raybet雷竞技最新j .raybet雷竞技最新气候11,676 - 689。[4.7]施耐德,N。, S. Venzke, A.J. Miller et al, 1999a: Pacific thermocline bridge revisited. Geophys. Res. Lett. 26, 1329-1332. [5.3] Schneider, N., A. J. Miller, M. A. Alexander and C. Deser, 1999b: Subduction of decadal North Pacific temperature anomalies: observations and dynamics. J. Phys. Oceanogr. 29, 1056-1070. [4.3, 4.4, 5.3, 5.4, 7.1] Schneider, R.J., G. A. Jones, A. P. McNichol et al., 1994: Methods for data screening, flagging, and error analysis at the National Ocean Sciences

AMS设备。核Instr。和方法。B92, 172 - 175。[5.8]Schopf,另外D.L.T.安德森和r .史密斯,1981:数据离差的低频罗斯比波。直流发电机大气压。海洋5,187 - 214。[4.4]Schopf,注:M.J.苏亚雷斯,1988:摇摆不定的海气耦合模式。j .大气压。 Sci. 45, 549-566. [3.3] Schott, F., 1983: Monsoon response of the Somali Current and associated upwelling. Prog. Oceanogr. 12, 357-381. [4.3] Schott, F., 1986: Seasonal variation of cross-equatorial flow in the Somali Current. J. Geophys. Res. 91, 10581-10584. [4.3] Schott, F. and C.W. Böning, 1991: Evaluation of the WOCE model in the western equatorial Atlantic: Upper-layer circulation. J. Geophys. Res. 96, 6993-7004. [4.3] Schott, F. and K. D. Leaman, 1991: Observations with moored Acoustic Doppler Current Profilers in the convection regime in the Golfe du Lion. J. Phys. Oceanogr. 21, 558-574. [5.5] Schott, F. and H. Stommel, 1978: Beta spirals and absolute velocities in different oceans. Deep-Sea Res. 25, 961-1010. [4.4] Schott, F.A., T.N. Lee and R. Zantopp, 1988: Variability of structure and transport of the Florida Current in the period range of days to seasonal. J. Phys. Oceanogr. 18, 1209-1230. [2.1] Schott, F., J.C. Swallow and M. Fieux, 1989: Deep currents underneath the equatorial Somali Current. Deep-Sea Res. 36, 1191-1199. [4.3] Schott, F., J.C. Swallow and M. Fieux, 1990: The Somali Current at the equator: Annual cycle of currents and transports in the upper 1000 m and connection to neighbouring latitudes. Deep-Sea Res. 37, 1825-1848. [4.3] Schott, F., J. Fischer, J. Reppin and U. Send, 1993a: On the mean and seasonal currents and transports at the western boundary of the equatorial Atlantic. J. Geophys. Res. 98, 14353-14368. [4.3, 4.5]

Schott F。m . Visbeck和j·费舍尔1993 b:观测的垂直水流和对流在中央格陵兰海在1988 - 1989年的冬天。j .地球物理学。研究》98年,14401 - 14421。^ [1.2,5.5]

Schott F。,J。Reppin, J. Fischer and D. Quadfasel, 1994: Currents and transports of the Monsoon Current south of Sri Lanka. J. Geophys. Res. 99, 25127-25141. Schott, F.A., L. Stramma and J. Fischer, 1995: The warm water inflow into the western tropical Atlantic boundary regime, spring 1994. J. Geophys. Res. 100, 24745-24760. [4.3]

Schott F。,m . Visbeck发送、j·菲舍尔l . Stramma和y Desaubies 1996:观测墨西哥湾的深对流的狮子,地中海北部,冬季的1991/92。期刊。Oceanogr。26日,505 - 524。(4.2,5.5,5.7)Schott, F。,J。Fischer, U. Garternicht and D. Quadfasel, 1997: Summer monsoon response of the northern Somali Current, 1995. Geophys. Res. Lett. 24, 2565-2568. [3.1, 4.3] Schott, F. A., J. Fischer and L. Stramma, 1998: Transports and pathways of the upper-layer circulation in the western tropical Atlantic. J. Phys. Oceanogr. 28, 1904-1928. [4.3, 4.7] Schott, F., Stramma, L. and J. Fischer, 1999: Interaction of the North Atlantic Current with the deep Charlie-Gibbs Fracture Zone throughflow. Geophys. Res. Lett. 26, 369-372. [5.6] Schott, G., 1928: Die Wasserbewegungen im Gebiete der Gibraltarstrasse. Journal du Conseil International pour l'Exploration de la mer. III, No. 2, Copenhagen, September. [5.7] Schröder, M. and E. Fahrbach, 1999: On the structure and the transport of the eastern Weddell Gyre. Deep-Sea Res. 46, 501-527. [4.6] Schroeder, E.H., H. Stommel, D.W. Menzel and W.H. Sutcliffe, Jr, 1959: Climate stability of eighteen degree water at Bermuda. J. Geophys. Res. 64, 363-366. [5.4] Schudlich, R. R. and J. F. Price, 1992: Diurnal cycles of turbulent dissipation, current and temperature in a model of the equatorial upper ocean. J. Phys. Oceanogr. 97, 5409-5422. [5.2] Schulz, J., P. Schlüssel and H. Grassl, 1993: Water vapor in the atmospheric boundary layer over oceans from SSM/I measurements. Int. J. Remote Sens. 14, 2773-2789. [3.4] Schulz, J., J. Meywerk, S. Ewald, and P. Schlüssel, 1997: Evaluation of satellite-derived latent heat fluxes. J. Climate, 10, 2782-2795. [3.4] SCOR, 1985: Oceanic CO2 measurements. Report of the Third Meeting of the Working Group 75, Les Houches, France, October 1985. [6.3] Seckmeyer, G., B. Mayer, G. Bernhard et al., 1995: Geographical differences in the UV measured by intercompared spectroradiometers. Geophys. Res. Lett. 22, 1889-1892. [1.1] Seidov, D. and B. Haupt, 1999: Last glacial and meltwater interbasin water exchanges and sedimentation in the world ocean. J. Phys. Oceanogr. 14, 760-769. [4.7] Sekine, Y. and K. Kutsuwada, 1994: Seasonal variation in volume transport of the Kuroshio south of Japan. J. Phys. Oceanogr. 24, 261-272. [2.2] Semtner, A.J. and R. M. Chervin, 1988: A simulation of the全球海洋环流解决涡流。j .地球物理学。研究》93年,15502 - 15522,15767 - 15775。[2.2]Semtner, a·j·r·m·谢尔文1992:从全球eddy-resolving海洋环流模式。j .地球物理学。研究》97年,5493 - 5550。(2.1,2.2,3.3,4.3,4.7,7.1]Semtner,抗干扰和y .明茨,1977:墨西哥湾流的数值模拟和中期海洋漩涡。期刊。Oceanogr。7, 208 - 230。[2.2]发送、U。,1994:Accuracy of current profile measurements: effect of tropical and midlatitude internal waves. J. Geophys. Res. 99, 16229-16236. [3.1] Send, U. and J. Marshall, 1995: Integral effects of deep convection. J. Phys. Oceanogr. 25, 855-872. [5.5] Send, U., F. Schott, F. Gaillard and Y. Desaubies, 1995: Observation of a deep convection regime with声波层析成象。j .地球物理学。研究》100年,6927 - 6941。[5.5]发送、U。r·韦勒,s·坎宁安et al ., 2001:海洋观测时间序列。:观察海洋在21世纪,n . r .史密斯和c . j . Koblinsky (eds)气象局,墨尔本,澳大利亚,24章。[7.4]Serreze,贝拉,J。A. Maslanik, J.R. Key, R.F. Kokaly and D. A. Robinson, 1995: Diagnosis of the record minimum in Arctic sea-ice area during 1990 and associated snow cover extremes. Geophys. Res. Lett. 22, 2183-2186. [7.3] Servain, J., 1991: Simple climatic indices for the tropical Atlantic Ocean and some applications. J. Geophys. Res. 96, 15137-15146. [4.3] Servain, J., A.J. Busalacchi, M.J. McPhaden et al., 1998: A Pilot Research Moored Array in the Tropical Atlantic (PIRATA). Bull. Amer. Meteor. Soc. 79, 2019-2031. [4.3, 7.4] Shchepetkin, A.F. and J.C. McWilliams, 1998: Quasi-monotonic advection schemes based on explicit locally adaptive dissipation. Mon. Wea. Rev. 126, 1541-1580. [7.2] Sherman, J. T. and R. E. Davis, 1995: Observations of temperature microstructure in NATRE. J. Phys. Oceanogr. 25, 1913-1929. [5.2] Shetye, S. R., S. S . C. Shenoi, A. D. Gouveia, G. S. Michael, D. Sundar and G. Nampoothori, 1991: Wind-driven海岸上涌沿着西部边界的孟加拉湾西南季风。Contin。架子上11号决议1397 - 1408。[4.3]Shin, s和z刘,2000:在赤道温跃层温带浮力强迫的响应。期刊。Oceanogr。2883 - 2905。[4.4]辛德尔,D.T.R.L.米勒,g·施密特和l . Pandolfo 1999:最近北方冬季气候趋势的模拟raybet雷竞技最新温室气体强迫。大自然399年,452 - 455。[2.3]

施赖弗参考书籍和赫尔伯特阁下,1997:的贡献全球温盐环流通过印尼太平洋到印度洋通流。j .地球物理学。研究》102年,5491 - 5511。[4.4,4.7]Shum c K。r·a·维尔纳·d·t·桑德维尔,林丙辉张,R.S. Nerem和最初Tapley 1990:全球变化的中尺度涡能量从地质卫星观测到的。j .地球物理学。研究》95年,17865 - 17876。[3.3]Shuto, K。,1996:水的温度和盐度年际变化在137°E子午线。j . Oceanogr。52岁,575 - 595。 [5.4] Siedler, G. and J.D. Woods (eds), 1980: GATE-1 oceanography and surface layer meteorology in the B/C scale. Deep-Sea Res. 26(suppl. 1), 294 pp. [1.3] Siedler, G., A. Kuhl and W. Zenk, 1987: The Madeira mode water. J. Phys. Oceanogr. 17, 1561-1570. [5.3, 5.4] Siedler, G., N. Zangenberg, R. Onken and A. Morliere, 1992: Seasonal changes in the tropical Atlantic circulation: observation and simulation of the Guinea Dome. J. Geophys. Res. 97, 703-715. [4.3] Siefridt, L., 1994: Validation des données de vent ERS-1 et des flux de surface du CEPMMT dans le context de la modélisation des circulations océaniques a léchelle d'un bassin. Ph.D. Thesis, Université约瑟夫傅里叶法国格勒诺布尔。[3.3]Siegenthaler, f·乔斯,1992:使用一个简单的模型为研究海洋示踪剂分布和全球碳循环。忒勒斯44 b, 186 - 207。[6.3]Siegenthaler,和j·l·Sarmiento 1993:大气二氧化碳和海洋。大自然365年,119 - 125。[6.3]Sjoberg, b和a . Stigebrandt 1992:地理分布的能量通量的计算通过内部潮汐和相关的混合过程垂直循环在海洋里。深海研究》39,269 - 291。[4.2]Slinn大桥街1999:内部反射波。:“啊哈Huliko传闻诉讼夏威夷冬季车间。海洋动力学内部重力波,二世。夏威夷大学Manou,嗨,1999年1月,p·穆勒和d·亨德森(eds), 141 - 147页。[5.2]Slinn, d . n和j·j·莱利,1999:内部波反射从倾斜的边界。j .流体机械。(提交)。 [5.2] Slocum, J., 1900: Sailing alone around the world. Century Company, New York and Sampson Low, London. Republished by Dover Publications, New York 1956, 294pp [3.2] Sloyan, B., 1997: The circulation of the southern ocean and the adjacent ocean basins determined by inverse methods. Ph.D. Thesis, Institute of

南极和南部海洋研究,塔斯马尼亚大学,479页。[7.1]Sloyan, b m和s . r . Rintoul 2000:估计area-averaged diapycnal通量从盆地规模预算。期刊。Oceanogr。2320 - 2341。[4.6,4.7]

Sloyan, B.M. S.R. Rintoul, 2001:全球深推翻南大洋肢体循环。期刊。Oceanogr。(提交)。[4.6,6.2]Sloyan, B.M. S.R. Rintoul, 2001 b:循环,南极模式和中间水的更新和修改。期刊。Oceanogr。(印刷中)。[4.6]

Smagorinsky,J。1963:环流实验与原始方程。我:基础实验。星期一,我们。91年启,99 - 164。[7.2]Smethie,瓦特计,1993:跟踪西北的温盐环流

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