| 1 |
dimitri |
1.1 |
@Article{Barnier:1995,
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| 2 |
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|
author = "Bernard Barnier and L. Siefridt and P. Marchesiello",
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| 3 |
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|
title = "Thermal Forcing for a Global Ocean Circulation Model
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| 4 |
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Using a Three-year Climatology of {ECMWF} analyses",
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| 5 |
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journal = jms,
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| 6 |
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year = 1995,
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| 7 |
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volume = 6,
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| 8 |
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pages = "363--380"
|
| 9 |
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}
|
| 10 |
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| 11 |
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@Article{Bersch:1995,
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| 12 |
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author = {Manfred Bersch},
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| 13 |
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title = {On the Circulation of the northeastern {N}orth
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| 14 |
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{A}tlantic},
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| 15 |
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journal = dsr,
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| 16 |
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year = 1995,
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| 17 |
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volume = 42,
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| 18 |
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number = 9,
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| 19 |
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pages = {1583--1607}
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| 20 |
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}
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| 21 |
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| 22 |
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@TechReport{Boyer:1994,
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| 23 |
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author = {T. P. Boyer and S. Levitus},
|
| 24 |
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title = {Quality control and processing of historical
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| 25 |
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oceanographic temperature, salinity, and oxygen
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| 26 |
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data.},
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| 27 |
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institution = {{NOAA}},
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| 28 |
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year = 1994,
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| 29 |
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type = {{NOAA} {A}tlas {S}eries},
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| 30 |
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number = {NESDIS 81},
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| 31 |
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address = {Washington, D.C.},
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| 32 |
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note = {64 pp.}
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| 33 |
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}
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| 34 |
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| 35 |
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@TechReport{Boyer:1997,
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| 36 |
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author = "T. P. Boyer and S. Levitus",
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| 37 |
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title = "Objective Analyses of Temperature and Salinity for
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| 38 |
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the Word Ocean on a 1/4 degree grid",
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| 39 |
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institution = "U.S. Gov. Printing Office, Washington, D.C.",
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| 40 |
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type = {{NOAA}/{NESDIS} {A}tlas},
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| 41 |
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year = 1997,
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| 42 |
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number = "11"
|
| 43 |
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}
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| 44 |
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| 45 |
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@Article{Bryden:1973,
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| 46 |
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author = "H. L. Bryden",
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| 47 |
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title = "New Polynomials for Thermal Expansion, Adiabatic
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| 48 |
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Temperature Gradient and Potential Temperature of
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| 49 |
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Sea Water",
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| 50 |
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journal = dsr,
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| 51 |
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year = 1973,
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| 52 |
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volume = 20,
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| 53 |
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pages = "401--408"
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| 54 |
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}
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| 55 |
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| 56 |
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@Article{Bryden:1991,
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| 57 |
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author = {Harry L. Bryden and Dean H. Roemmich and
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| 58 |
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John. A. Church},
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| 59 |
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title = {Ocean Heat Transport Across 24 Degree {N} in the
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| 60 |
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{P}acific},
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journal = dsr,
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year = 1991,
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| 63 |
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volume = 38,
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| 64 |
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number = {3A},
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| 65 |
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pages = {397--324}
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| 66 |
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}
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| 67 |
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@InCollection{Bryden:93,
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author = "H. L. Bryden",
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title = "Ocean Heat Transport Across {24$^{\circ}$N} Latitude",
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publisher = "American Geophysical Union",
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year = 1993,
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editor = "G. A. {McBean} and M. Hantel",
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volume = 75,
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series = "{AGU} Geophysical Monograph",
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pages = "65-75",
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address = "Washington, DC"
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}
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@Article{Chelton:1990,
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author = "D. B. Chelton and Mestas-Nu{\~n}ez and
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F. J. Freilich",
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title = "Global Wind Stress and {S}verdrup Circulation from
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the {S}easat Scatterometer",
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year = 1990,
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volume = 20,
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author = {A. Defant},
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title = {{Q}uantitative {U}ntersuchungen zur {S}tatik und
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{D}ynamik des {A}tlantischen {O}zeans. {D}ie
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absolute {T}opographie des physikalischen
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| 97 |
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{M}eeresniveaus und der {D}ruckfl{\"a}chen sowie die
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| 98 |
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{W}asserbewegungen im {R}aum des {A}tlantischen
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{O}zeans},
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booktitle = {{W}issenschaftliche {E}rgebnisse der {D}eutschen
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{A}tlantischen {E}xpedition auf dem {F}orschungs-
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pages = {191--260},
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year = 1941,
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volume = {6:2}
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}
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@TechReport{Fofonoff:1983,
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author = "Fofonoff, P. and Millard, Jr., R.C.",
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| 111 |
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title = "Algorithms for Computation of Fundamental Properties
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| 112 |
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of Seawater",
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institution = "Unesco",
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| 114 |
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year = 1983,
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type = "Unesco Technical Papers in Marine Science",
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| 116 |
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number = 44,
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pages = {53 pp.}
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| 118 |
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}
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@Book{Gill:1982,
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| 121 |
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author = {Adrian E. Gill},
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| 122 |
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title = {Atmosphere-Ocean Dynamics},
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publisher = {Academic Press},
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year = 1982,
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volume = 30,
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pages = {666},
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| 127 |
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series = {International Geophysics Series}
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}
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@Article{Hidaka:1940a,
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| 131 |
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author = {K. Hidaka},
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| 132 |
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title = {Absolute Evaluation of Ocean Currents in Dynamic
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| 133 |
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Calculations},
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| 134 |
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journal = piat,
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year = 1940,
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volume = 16,
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pages = {391--393}
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}
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@Article{Hidaka:1940b,
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author = {K. Hidaka},
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| 142 |
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title = {Practial Evaluation of Ocean Currents},
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| 143 |
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journal = piat,
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year = 1940,
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volume = 16,
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pages = {394--397}
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}
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@TechReport{Levitus:1994a,
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author = {S. Levitus and T.P. Boyer},
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title = {{W}orld {O}cean {A}tlas 1994. {V}olume 2: {O}xygen},
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institution = {{NOAA}},
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year = 1994,
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type = {{NOAA} {A}tlas {NEDSIS}},
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address = {Washington D.C.},
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number = {2}
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}
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@TechReport{Levitus:1994b,
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author = {S. Levitus and R. Burgett and T.P. Boyer},
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title = {{W}orld {O}cean {A}tlas 1994. {V}olume 3: {S}alinity},
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institution = {{NOAA}},
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| 163 |
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year = 1994,
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type = {{NOAA} {A}tlas {NEDSIS}},
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address = {Washington D.C.},
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number = {3},
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pages = {99}
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}
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@TechReport{Levitus:1994c,
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author = {S. Levitus and T.P. Boyer},
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title = {{W}orld {O}cean {A}tlas 1994. {V}olume 4: {T}emperature},
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institution = {{NOAA}},
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year = 1994,
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type = {{NOAA} {A}tlas {NEDSIS}},
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address = {Washington D.C.},
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number = {4},
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pages = {117}
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}
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@Article{Millero:1980,
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author = "Millero, F.J. and Chen, C.T. and Bradshaw, A. and
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Schleicher, K.",
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title = "A New High Pressure Equation of State for Seawater",
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year = 1980,
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volume = "27A",
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}
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@Book{Pedlosky:1986,
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author = {Joseph Pedlosky},
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title = {Geophysical Fluid Dynamics},
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publisher = {Springer},
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year = 1987,
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address = {New York},
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}
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@Proceedings{WissErgebMeteor:1927,
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title = {{W}issenschaftliche {E}rgebnisse der {D}eutschen
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{A}tlantischen {E}xpedition auf dem {F}orschungs-
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und {V}ermessungsschiff {``Meteor''}},
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year = {1925--1927},
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}
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@Book{Worthington:1976,
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author = {L. V. Worthington},
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title = {On the {N}orth {A}tlantic Circulation},
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publisher = {Johns Hopkins University Press},
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year = 1976,
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address = {Baltimore}
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}
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title = {{S}chichtung und {Z}irkulation des {A}tlantischen
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{O}zeans. {D}as {B}odenwasser und die {S}tratosph{\"a}re},
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booktitle = {{W}issenschaftliche {E}rgebnisse der {D}eutschen
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{A}tlantischen {E}xpedition auf dem {F}orschungs-
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pages = {1--288},
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year = 1935,
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volume = {6:1, 2},
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}
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@Article{adcroft01:_geoth_heating_global_ocean_circul,
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author = {Alistair Adcroft and Jeffery R. Scott and Jochem
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Marotzke},
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title = {Impact of Geothermal Heating on the Global Ocean
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Circulation},
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}
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@Article{adcroft98:_slippery_coast,
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author = {Alistair Adcroft and David Marshall},
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title = {How Slippery are Piecewise-Constant Coastlines in
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Numerical Ocean Models?},
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year = 1998,
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}
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author = {Mark Rosenberg and Ruth Eriksen and Stephen Rintoul},
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title = {{A}urora {A}ustralis Marine Science Cruise
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{AU9309/AU9391} - Oceanographic Field Measurements
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and Analysis},
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institution = {Antarctic {CRC}},
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type = {{A}ntarctic {CRC} Research Report},
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number = 2,
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}
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@TechReport{au9404,
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author = {Mark Rosenberg and Ruth Eriksen and Steve Bell and
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| 264 |
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Stephen Rintoul},
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title = {{A}urora {A}ustralis Marine Science Cruise {AU9404}
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- Oceanographic Field Measurements and Analysis},
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institution = {Antarctic {CRC}},
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type = {{A}ntarctic {CRC} Research Report},
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}
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@TechReport{au9407,
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author = {Mark Rosenberg and Ruth Eriksen and Steve Bell and
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Nathan Bindoff and Stephen Rintoul},
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title = {{A}urora {A}ustralis Marine Science Cruise {AU9407}
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- Oceanographic Field Measurements and Analysis},
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institution = {Antarctic {CRC}},
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type = {{A}ntarctic {CRC} Research Report},
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number = 6,
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address = {Hobart, Australia}
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}
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@TechReport{au9604,
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author = {Mark Rosenberg and Stephen Bray and Nathan Bindoff
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and Stephen Rintoul and Neale Johnston and Steve Bell
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| 289 |
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and Phillip Towler},
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title = {{A}urora {A}ustralis Marine Science Cruise {AU9407}
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- Oceanographic Field Measurements and Analysis,
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Intercruise Comparisons and Data Quality Notes},
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institution = {Antarctic {CRC}},
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year = 1997,
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type = {{A}ntarctic {CRC} Research Report},
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number = 12,
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}
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@Unpublished{barnard:_dynamo,
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author = {Sally Barnard and Bernard Barnier and Aike Beckmann
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and Claus W. B{\"o}ning and Macky Coulibaly and
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D'Arcy DeCuevas and Joachim Dengg and Christian
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Dieterich and Ute Ernst and Peter Herrmann and Yanli
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Jia and Peter D. Killworth and J{\"u}rgen Kr{\"o}ger
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and Mei-Man Lee and Christian LeProvost and
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Jean-Marc Molines and Adrian L. New and Andreas
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Oschlies and Thierry Reynaud and Luke J. West and
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J{\"u}rgen Willebrand},
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title = {{DYNAMO}, {D}ynamics of {N}orth {A}tlantic {M}odels},
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note = {{DYNAMO} Scientific Report {N$^o$3}},
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year = {1997}
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}
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@Article{beckmann97,
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author = {Aike Beckmann and Ralf Doescher},
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title = {A Method for Improved Representation of Dense Water
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Spreading over Topography in Geopotential-Coordinate
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Models},
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journal = jpo,
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year = 1997,
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volume = 27,
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}
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@Article{beismann04,
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author = {Jens-Olaf Beismann and Bernard Barnier},
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title = {Variability of the Meridional Overturning
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Circulation of the {N}orth {A}tlantic: Sensitivity
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to Overflows of Dense Water Masses},
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journal = {Ocean Dynamics},
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}
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number = 6,
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|
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}
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Martin Schmidt and V. Balaji},
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| 684 |
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title = {Tracer Conservation with an Explicit Free Surface
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}
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title = {Optimal Fingerprints for the Detection of
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Time-dependent Climate Change},
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title = {Conventional and {B}ayesian Approach to
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Climate-Change Detection and Attribution},
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abstract = {The conventional multi-variate, multi-fingerprint
|
| 733 |
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|
theory of climate-change detection and attribution,
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| 734 |
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|
expressed in terms of existing frequency
|
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distributions, is reviewed and generalized to a
|
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Bayesian approach based on subjective
|
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probabilities. Bayesian statistics enable a
|
| 738 |
|
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quantitive determination of the impact of
|
| 739 |
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|
climate-change detection tests on prior subjective
|
| 740 |
|
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assessments of the probability of an externally
|
| 741 |
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forced climate change. The Bayesian method also
|
| 742 |
|
|
provides a potentially powerful tool for enhancing
|
| 743 |
|
|
statistical detection and attribution tests by
|
| 744 |
|
|
combining a number of different climate-change
|
| 745 |
|
|
indicators that are not amenable to standard
|
| 746 |
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|
signal-to-noise analyses because of inadequate
|
| 747 |
|
|
information on the associated natural-variability
|
| 748 |
|
|
statistics. The relation between the conventional
|
| 749 |
|
|
and Bayesian approach is illustrated by examples
|
| 750 |
|
|
taken from recent conventional analyses of
|
| 751 |
|
|
climate-change detection and attribution for three
|
| 752 |
|
|
cases of climate-change forcing by increasing
|
| 753 |
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|
greenhouse-gas concentrations, increasing
|
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greenhouse-gas and aerosol concentrations, and
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variations in solar insolation. The enhancement of
|
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|
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detection and attribution levels through a joint
|
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|
Bayesian analysis of a number of different
|
| 758 |
|
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climate-change indices is demonstrated in a further
|
| 759 |
|
|
example. However, this advantage of the Bayesian
|
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approach can be achieved only within the framework
|
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of a subjective rather than objective analysis. The
|
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conventional and Bayesian approach both exhibit
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specific advantages and shortcomings, so that a
|
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parallel application of both methods is probably the
|
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title = {An Assessment of the {G}eophysical {F}luid
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Krauss and Gerold Siedler",
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title = "Allgemeine Meereskunde",
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year = 1975,
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pages = "594",
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W. Collins and D. Deaven and L. Gandin and
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M. Iredell and S. Saha and G. White and J. Woollen
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W. Higgins and J. Janowiak and K. C. Mo and
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C. Ropelewski and J. Wang and A. Leetmaa and
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R. Reynolds and R. Jenne and D. Joseph},
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title = {The {NMC/NCAR} 40-Year Reanalysis Project},
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year = 1996,
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author = {Peter D. Killworth and Neil R. Edwards},
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title = {A Turbulent Bottom Boundary Layer Code for Use in
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Numerical Ocean Models},
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volume = 29,
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@TechReport{king94:_altim_data_set,
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author = {Charmaine King and Detlef Stammer and Carl Wunsch},
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title = {The {CMPO/MIT} {TOPEX/POSEIDON} Altimetric Data Set},
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institution = {Center of Global Change Science, Massachusetts
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Institute of Technology},
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year = 1994,
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type = {Report},
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number = 30
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}
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@Article{kistler01,
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author = {R. Kistler and E. Kalnay and W. Collins and S. Saha
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and G. White and J. Woollen and M. Chelliah and
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W. Ebisuzaki and M. Kanamitsu and V. Kousky and
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H. van den Dool and R. Jenne and M. Fiorino},
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title = {The {NCEP-NCAR} 50-Year Reanalysis: Monthly Means
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{CD-ROM} and Documentation},
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title = {The Transport of the {W}eddell {G}yre Across the
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author = {Gert K{\"o}nig-Langlo and Ernst Augstein},
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title = {Parameterization of the Downward Long-Wave Radiation
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at the {E}arth's Surface in Polar Regions},
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title = {The Meteorological Information System at the
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@Book{kowalik93:_num_mod,
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title = {Diurnal to decadal global forcing for ocean and
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@Article{madec91,
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title = {A Three-Dimensional Numerical Study of Deep-Water
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Formation in the {N}orthwestern {M}editerranean
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{S}ea},
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@Article{marks06,
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author = {K. M. Marks and W. H. F. Smith},
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detection is successful, attribution of the observed
|
| 1345 |
|
|
climate change to the hypothesized forcing mechanism
|
| 1346 |
|
|
is carried out in a second step by comparing the
|
| 1347 |
|
|
observed and predicted climate change signals. In
|
| 1348 |
|
|
contrast, the Bayesian approach to detection and
|
| 1349 |
|
|
attribution makes no distinction between detection
|
| 1350 |
|
|
and attribution. The purpose of filtering in this
|
| 1351 |
|
|
case is to maximize the impact of the evidence, the
|
| 1352 |
|
|
observed climate change, on the prior probability
|
| 1353 |
|
|
that the hypothesis of an anthropogenic origin of
|
| 1354 |
|
|
the observed signal is true. Whereas in the
|
| 1355 |
|
|
conventional approach model uncertainties have no
|
| 1356 |
|
|
direct impact on the definition of the optimal
|
| 1357 |
|
|
detection fingerprint, in optimal Bayesian filtering
|
| 1358 |
|
|
they play a central role. The number of patterns
|
| 1359 |
|
|
retained is governed by the magnitude of the
|
| 1360 |
|
|
predicted signal relative to the model
|
| 1361 |
|
|
uncertainties, defined in a pattern space normalized
|
| 1362 |
|
|
by the natural climate variability. Although this
|
| 1363 |
|
|
results in some reduction of the original phase
|
| 1364 |
|
|
space, this is not the primary objective of Bayesian
|
| 1365 |
|
|
filtering, in contrast to the conventional approach,
|
| 1366 |
|
|
in which dimensional reduction is a necessary
|
| 1367 |
|
|
prerequisite for enhancing the signal-to-noise
|
| 1368 |
|
|
ratio. The Bayesian filtering method is illustrated
|
| 1369 |
|
|
for two anthropogenic forcing hypotheses: greenhouse
|
| 1370 |
|
|
gases alone, and a combination of greenhouse gases
|
| 1371 |
|
|
plus sulfate aerosols. The hypotheses are tested
|
| 1372 |
|
|
against 31-year trends for near-surface temperature,
|
| 1373 |
|
|
summer and winter diurnal temperature range, and
|
| 1374 |
|
|
precipitation. Between six and thirteen response
|
| 1375 |
|
|
patterns can be retained, as compared with the one
|
| 1376 |
|
|
or two response patterns normally used in the
|
| 1377 |
|
|
conventional approach. Strong evidence is found for
|
| 1378 |
|
|
the detection of an anthropogenic climate change in
|
| 1379 |
|
|
temperature, with some preference given to the
|
| 1380 |
|
|
combined forcing hypothesis. Detection of recent
|
| 1381 |
|
|
anthropogenic trends in diurnal temperature range
|
| 1382 |
|
|
and precipitation is not successful, but there
|
| 1383 |
|
|
remains strong net evidence for anthropogenic
|
| 1384 |
|
|
climate change if all data are considered jointly.}
|
| 1385 |
|
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}
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| 1386 |
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|
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@Article{schodlok02,
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Beckmann},
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title = {On the Transport, Variability and Origin of Dense
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Water Masses Crossing the {S}outh {S}cotia {R}idge},
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}
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