Preface |
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xiii | |
Acknowledgments |
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xvii | |
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1 | (32) |
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2 | (11) |
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The last 2.5 million years |
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3 | (2) |
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5 | (3) |
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8 | (1) |
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Causes of past climate variability |
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9 | (4) |
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The Present Ocean Circulation |
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13 | (8) |
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13 | (2) |
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Ocean circulation patterns |
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15 | (3) |
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Heat and freshwater transport |
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18 | (1) |
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Ocean circulation and past climate variability |
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19 | (2) |
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Present Climate Variability |
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21 | (6) |
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22 | (3) |
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North Atlantic interdecadal variability |
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25 | (2) |
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Physics of Climate Variability |
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27 | (6) |
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27 | (2) |
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29 | (1) |
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30 | (3) |
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33 | (22) |
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34 | (9) |
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34 | (2) |
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36 | (2) |
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38 | (2) |
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40 | (1) |
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41 | (2) |
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43 | (4) |
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47 | (3) |
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50 | (5) |
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A Dynamical Systems Point of View |
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55 | (50) |
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56 | (11) |
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The Stommel two-box model |
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57 | (3) |
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60 | (2) |
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Stability of equilibrium solutions |
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62 | (1) |
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63 | (3) |
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66 | (1) |
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Dynamical Systems: Fixed Points |
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67 | (13) |
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67 | (3) |
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Codimension-1 bifurcations |
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70 | (1) |
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71 | (3) |
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A single complex pair of eigenvalues |
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74 | (1) |
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75 | (3) |
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Codimension-2 bifurcations |
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78 | (2) |
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Periodic Solutions and their Stability |
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80 | (8) |
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Poincare section and Poincare map |
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80 | (5) |
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85 | (3) |
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Bifurcations of Periodic Orbits |
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88 | (8) |
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Destabilization of periodic orbits |
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89 | (2) |
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91 | (2) |
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93 | (3) |
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Physics of Bifurcation Behavior |
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96 | (9) |
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Physical constraints and bifurcation diagrams |
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96 | (1) |
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Qualitative versus quantitative sensitivity |
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97 | (3) |
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100 | (1) |
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100 | (1) |
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Transcritical and pitchfork bifurcation |
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101 | (1) |
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102 | (3) |
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105 | (46) |
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108 | (5) |
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108 | (1) |
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109 | (2) |
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111 | (1) |
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Non-dimensional equations |
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112 | (1) |
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Computation of Steady Solutions |
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113 | (7) |
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113 | (3) |
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Pseudo-arclength continuation |
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116 | (2) |
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118 | (2) |
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Detection and Branch Switching |
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120 | (4) |
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Detection of bifurcations |
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120 | (2) |
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122 | (2) |
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124 | (8) |
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The simultaneous iteration method |
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126 | (3) |
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The Jacobi-Davidson QZ-method |
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129 | (3) |
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Implicit Time Integration |
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132 | (1) |
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Linear System Solvers: Direct Methods |
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133 | (3) |
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133 | (2) |
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135 | (1) |
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Linear System Solvers: Iterative Methods |
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136 | (8) |
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136 | (2) |
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138 | (1) |
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139 | (1) |
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140 | (2) |
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142 | (2) |
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Application to the Prototype Problem |
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144 | (7) |
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The Wind-Driven Ocean Circulation |
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151 | (74) |
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152 | (5) |
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152 | (2) |
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154 | (2) |
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156 | (1) |
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Models of the Midlatitude Ocean Circulation |
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157 | (6) |
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157 | (2) |
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159 | (2) |
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161 | (2) |
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Intermediate Complexity Models |
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163 | (7) |
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163 | (1) |
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164 | (3) |
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Quasi-geostrophic β-plane models |
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167 | (2) |
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Overview of the intermediate models |
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169 | (1) |
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170 | (14) |
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The Sverdrup-Munk-Stommel theory |
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171 | (4) |
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175 | (1) |
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175 | (1) |
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176 | (2) |
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Basic instability mechanisms |
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178 | (6) |
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Flows in Small Rectangular Basins |
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184 | (18) |
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Quasi-geostrophic barotropic flows |
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184 | (8) |
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192 | (3) |
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The (equivalent) barotropic shallow water case |
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195 | (5) |
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Connection: SW- and QG-models |
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200 | (2) |
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202 | (8) |
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Continents within a β-plane model |
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203 | (1) |
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204 | (4) |
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208 | (2) |
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210 | (6) |
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211 | (2) |
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Gulf Stream separation in POCM |
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213 | (3) |
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Temporal variability in POCM |
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216 | (1) |
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216 | (3) |
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Signatures of different separation patterns? |
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216 | (3) |
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219 | (1) |
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219 | (6) |
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221 | (1) |
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222 | (1) |
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222 | (3) |
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The Thermohaline Ocean Circulation |
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225 | (96) |
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226 | (5) |
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226 | (1) |
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227 | (4) |
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Central questions and approach |
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231 | (1) |
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231 | (9) |
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232 | (1) |
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233 | (3) |
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The flip-flop oscillation |
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236 | (2) |
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238 | (1) |
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Models of the thermohaline circulation |
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239 | (1) |
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Two-dimensional Boussinesq Models |
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240 | (3) |
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240 | (2) |
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242 | (1) |
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Diffusive Thermohaline Flows |
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243 | (25) |
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Basic bifurcation diagram |
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243 | (4) |
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247 | (1) |
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247 | (2) |
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Transition to time-dependence |
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249 | (3) |
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252 | (6) |
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Imperfections: flux-correction |
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258 | (3) |
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261 | (3) |
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Flux-correction procedure |
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264 | (1) |
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Solutions under flux-correction |
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264 | (4) |
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268 | (1) |
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Convective Thermohaline Flows |
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268 | (11) |
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Basic bifurcation diagrams |
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269 | (3) |
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272 | (1) |
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273 | (1) |
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Asymmetric air sea interaction |
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274 | (3) |
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277 | (2) |
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279 | (14) |
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280 | (2) |
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282 | (1) |
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283 | (3) |
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286 | (1) |
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The 'geostrophic' closure |
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287 | (4) |
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291 | (2) |
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293 | (5) |
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298 | (19) |
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299 | (1) |
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299 | (4) |
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303 | (1) |
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304 | (2) |
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Centennial (and longer) time scale |
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306 | (2) |
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308 | (3) |
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311 | (3) |
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Coupled ocean-atmosphere models |
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314 | (3) |
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317 | (4) |
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Different mean thermohaline flows? |
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317 | (2) |
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Temporal variability through instabilities? |
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319 | (2) |
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The Dynamics and Physics of ENSO |
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321 | (105) |
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322 | (9) |
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323 | (1) |
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324 | (3) |
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327 | (3) |
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Central questions and Approach |
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330 | (1) |
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Models of the Equatorial Ocean |
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331 | (14) |
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Constant density ocean model |
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331 | (1) |
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The reduced gravity model |
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332 | (2) |
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334 | (4) |
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Forced response in a basin |
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338 | (7) |
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345 | (14) |
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Atmospheric response to diabatic heating |
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345 | (5) |
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350 | (4) |
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Processes determining the SST |
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354 | (2) |
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356 | (1) |
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356 | (2) |
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358 | (1) |
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Strength of the feedbacks |
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358 | (1) |
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359 | (6) |
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359 | (3) |
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362 | (3) |
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Towards the Delayed Oscillator |
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365 | (29) |
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Coupled modes: periodic ocean basin |
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365 | (5) |
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Coupled modes: bounded basin |
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370 | (1) |
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The near equatorial behavior |
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371 | (5) |
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376 | (3) |
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379 | (2) |
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Modes in the full problem |
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381 | (5) |
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Conceptual models of the ENSO oscillation |
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386 | (1) |
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386 | (3) |
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389 | (3) |
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The coupled wave oscillator |
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392 | (1) |
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392 | (2) |
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Coupled Processes and the Annual Mean State |
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394 | (10) |
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Constructed versus coupled mean states |
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394 | (1) |
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Demise of multiple equilibria |
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395 | (4) |
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The position of the cold tongue |
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399 | (5) |
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Unifying Mean State and Variability |
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404 | (8) |
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The warm pool/cold tongue state |
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404 | (2) |
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406 | (5) |
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411 | (1) |
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Presence of the Seasonal Cycle |
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412 | (10) |
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Coupled processes and the seasonal cycle |
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413 | (1) |
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Interaction of seasonal cycle and ENSO |
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414 | (5) |
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419 | (3) |
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422 | (4) |
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Simulation of the mean state |
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422 | (4) |
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426 | |