: Hendrik M. van Aken
: The Oceanic Thermohaline Circulation An Introduction
: Springer-Verlag
: 9780387480398
: 1
: CHF 139.30
:
: Geografie
: English
: 326
: Wasserzeichen
: PC/MAC/eReader/Tablet
: PDF

This book presents a global hydrographic description of the thermohaline circulation, an introduction to the theoretical aspects of this phenomenon, and observational evidence for the theory. The hydrographic description and the observational evidence are based on data sources available via internet, mainly from the World Oceanographic Experiment (WOCE). The book also offers an introduction to hydrographic analysis and interpretation.



 Dr. Hendrik van Aken has been an observational oceanographer for over 25 years. He mainly deals with regional oceanography. He headed the Dutch contribution ot the WOCE Hydrographic Program (WHP), and is presently active in CLIVAR projects. Dr. Van Aken has done extensive research in the fields of climate hydrographic variability and aspects of the global thermohaline  circulation.
Preface7
Contents10
List of Abbreviations13
1. Introduction16
1.1. Climate and climate variations16
1.2. The ocean and climate18
1.3. What is the THC?21
1.4. Some historical notes24
1.5. The following chapters28
2. The ocean basins30
2.1. The bottom topography of the oceans30
2.2. Basins and ridges31
3. Pressure, temperature, salinity, and some thermohaline dynamics35
3.1. Pressure35
3.2. Temperature37
3.3. Salinity38
3.4. Density40
3.5. Adiabatic compression, potential temperature, and potential density43
3.6. Freezing point and specific heat45
3.7. Pressure gradient forces47
3.8. Geostrophic and near-geostrophic flow49
3.9. Friction and transport52
3.10. Vertical motion and mass conservation54
4. Water mass and tracer analysis of the deep flow in the Atlantic Ocean59
4.1. Meridional sections of temperature, salinity and density59
4.2. Deriving the deep circulation from tracer distributions63
4.3. Wüst's core method65
4.4. Water mass, water type, and the temperature68
4.5. Quantitative water mass analysis72
4.6. The use of biogeochemical tracers75
4.7. Biogeochemical tracers in the Atlantic Ocean80
4.8. A natural radioactive tracer: radiocarbon83
4.9. Halocarbons as tracers86
4.10. Zonal hydrographic sections in the Atlantic Ocean89
5. The deep flow in the Southern, Indian, and Pacific oceans93
5.1. Hydrography of the Southern Ocean93
5.2. The deep Indian Ocean101
5.3. The hydrography of the deep Pacific Ocean107
5.4. Deep upwelling115
6. The upper branch of the THC117
6.1. Interocean exchange117
6.2. The Bering Strait through-flow118
6.3. The Indonesian through-flow120
6.4. The cold water route126
6.5. Return flow into the Arctic seas132
7. Formation and descent of water masses135
7.1. Water mass formation135
7.2. The Barents Sea136
7.3. A scheme for deep convection139
7.4. Deep convection in the Greenland Sea141
7.5. Norwegian Sea Deep Water145
7.6. Exchange between the Nordic seas and the North Atlantic Ocean146
7.7. Convection in the Labrador Sea152
7.8. Bottom water formation in the Southern Ocean156
8. Dynamics of the THC166
8.1. Meridional overturning circulation166
8.2. Upwelling and divergence of the abyssal circulation174
8.3. Geostrophic flow in the abyssal ocean176
8.4. Deep boundary currents179
8.5. Topographic influence on the abyssal circulation183
8.6. Observational evidence for the abyssal circulation scheme185
8.7. Wind-driven deep upwelling in the Southern Ocean196
9. Deep upwelling and mixing199
9.1. Profiles of conservative tracers199
9.2. Profiles of a tracer with first-order decay: radiocarbon203
9.3. Tracers with zeroth order sources and sinks: oxygen, and nutrients208
9.4. Energy requirements for turbulent mixing210
10. Energetics of the THC216
10.1. Some thermodynamics216
10.2. Heat exchange with the atmosphere and heat fluxes219
10.3. The influence of the hydrological cycle225
10.4. The density boundary conditions230
10.5. The THC engine and Sandström's theorem232
11. Simple models, boundary conditions, and feedbacks239
11.1. Models and boundary conditions239
11.2. Random boundary conditions241
11.3. Boundary conditions for temperature and salinity with feedback243
11.4. A consequence of SST-dependent evaporation247
11.5. Consequences of restoring boundary conditions248
11.6. The single-hemispheric Stommel box model252
11.7. The interhemispheric Rooth box model258
11.8. The stability of Rooth's model265
11.9. Two-dimensional meridional models of the THC270
11.10. Three-dimensional ocean general circulation models275
12. The THC and different climates279
12.1. Climate variability in numerical simulations279
12.2. Paleoclimate changes285
12.3. The past THC from oxygen isotopes in marine sediments289
12.4. Stable carbon isotopes and the Atlantic paleo-THC294
12.5. Cadmium and barium as paleoceanographic tracers of the THC301
12.6. Stable carbon isotopes in the Southern Ocean304
12.7. Global water mass changes in the deep ocean306
12.8. Ocean ventilation age from radiocarbon in sediment cores307
12.9. A model interpretation of proxy data311
References315
Index330