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9780444503381

Modeling the Earth's Climate and Its Variability

by ; ;
  • ISBN13:

    9780444503381

  • ISBN10:

    0444503382

  • Format: Hardcover
  • Copyright: 1999-12-13
  • Publisher: Elsevier Science
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Summary

Understanding and predicting the Earth's climate system, particularly climate variability and possible human-induced climate change, presents one of the most difficult and urgent challenges in science. Climate scientists worldwide have responded to that challenge over the past decade by creating a wide variety of ever more sophisticated climate models that are beginning to show considerable ability to replicate many aspects of the climate system. At the same time, to fully understand climate change, one also has to look to past climates. For this purpose five eminent scholars who span the disciplines of modeling and observation, including elements of past, present and future climate studies came together at this Les Houches school. They presented a systematic development of each of their respective subjects which provided a comprehensive overview of this vast and complex subject. These core lectures were supplemented by a set of shorter lectures and of seminars.

Table of Contents

Organizers ix
Lecturers xi
Seminar Speakers xiii
Participants xv
Preface (French) xxi
Preface (English) xxv
MAIN COURSES
The Observed Climate of the 20th Century
1(138)
E.M. Rasmusson
M. Chelliah
C.F. Ropelewski
Climatology: From statistics to science
5(13)
The evolution of climate science
5(3)
Characteristics and limitations of the instrumental data bases
8(7)
Interannual to interdecadal variability
15(2)
Modern climate diagnostics
17(1)
The atmospheric general circulation
18(17)
From Hadley to the mid-20th century: Theory underconstrained by observations
20(4)
Post-World War II: Resolving the controversies
24(1)
Quantifying the balance requirements
25(1)
Angular momentum balance
25(2)
Atmospheric energy cycle
27(2)
Planetary heat balance
29(3)
Hydrologic cycle
32(3)
The annual cycle
35(26)
Basic controls
43(9)
Focus on the tropics
52(4)
A monsoon system perspective
56(1)
Focus on the extratropics
57(4)
Interannual variability
61(38)
Atmospheric teleconnections
62(5)
The ENSO phenomenon: Early investigations
67(4)
ENSO cycle time series
71(1)
ENSO warm episode evolution
72(16)
ENSO global response
88(1)
Tropical anomalies
88(10)
Extratropical anomalies
98(1)
Decadal/interdecadal variability
99(40)
Focus on the tropical oceans
102(1)
Pacific sector
102(2)
Atlantic sector
104(1)
Focus on the extratropics
105(1)
Northern Hemisphere wintertime temperatures: relationship to the SO and the NAO
105(6)
North Atlantic and North Pacific
111(8)
Continental precipitation variability
119(1)
Sahel rainfall
120(6)
North American drought
126(1)
Indian rainfall
127(1)
Concluding remarks
128(1)
References
129(10)
Numerical Modelling of the Earth's Climate
139(98)
L. Bengtsson
A strategic approach to climate modelling
143(8)
Introduction
143(1)
Dynamics of climate
144(1)
Phillips' experiment
145(1)
The key scientific issues in 1955
146(1)
Climate modelling for different time-scales
147(4)
Climate modelling
151(15)
Introduction
151(2)
The climate model as a mathematical system
153(3)
Overall design of an atmospheric climate model
156(2)
Numerical solution
158(2)
Physical parameterization
160(2)
Climate model performance
162(4)
An atmospheric model for climate simulation and prediction studies
166(29)
Introduction
166(1)
Horizontal diffusion
167(1)
Surface fluxes and vertical diffusion
168(4)
Land surface processes
172(1)
Gravity wave drag
172(2)
Cumulus convection
174(1)
Adjustment closure
174(2)
Stratiform clouds
176(2)
Radiation
178(1)
Longwave radiation
178(3)
Shortwave radiation
181(4)
Shortwave cloud optical properties
185(1)
Longwave cloud optical properties
186(1)
Effective radii of cloud droplets and ice crystals
187(1)
Surface albedo
188(1)
Solar zenith angle
188(1)
Model validation
188(1)
Radiation and clouds
189(2)
The hydrological cycle
191(1)
The large scale extra-tropical circulation
192(3)
Climate response to greenhouse gas forcing
195(14)
Introduction
195(3)
Climate feedback processes
198(2)
The Wonderland climate model
200(3)
Forcing experiments with the Wonderland model
203(1)
Response to 2 x CO2 and 2% solar forcing
204(1)
Response to the horizontal and vertical distribution of the forcing
205(2)
Forcing experiments with more realistic climate models
207(2)
Climate change prediction
209(28)
Introduction
209(3)
Mechanisms behind climate change
212(1)
How can climate change?
212(1)
Changes in the solar radiation
212(1)
Changes in the greenhouse gases
213(1)
Changes in atmospheric aerosols
214(1)
Internal, natural variations
215(2)
Coupled models
217(4)
Coupled model experiments
221(1)
Transient greenhouse gas experiment
222(1)
Changes in the energy cycle
223(2)
The hydrological cycle
225(2)
Temperature changes
227(3)
References
230(7)
Ocean Modelling and the Role of the Ocean in the Climate System
237(78)
P. Delecluse
G. Madec
Physical properties of the ocean
241(8)
General structure
241(1)
Why does the ocean move?
241(1)
Radiative forcing
241(2)
Momentum flux
243(1)
Turbulent fluxes
244(2)
Freshwater flux
246(1)
Mean vertical structure
247(1)
Seasonal cycle of the mixed layer
247(1)
Midlatitude thermocline ventilation
247(1)
Equatorial thermocline
247(1)
Deep convection and sea ice
248(1)
Turbulence of the ocean
249(1)
Equations of motion
249(6)
The physical equations
249(1)
Basic assumptions (refer to Pedlosky, 1987)
249(1)
The Primitive Equations
250(1)
The boundary conditions
251(1)
Horizontal pressure gradient formulation
252(1)
Pressure formulation
252(1)
Diagnosing the surface pressure gradient
253(1)
Boundary conditions
254(1)
Modelling approach
255(22)
System of coordinates
255(1)
Model equations
256(2)
Vertical system of coordinates
258(1)
Meridian convergence at the pole
259(1)
Discretization in space
260(1)
Arrangement of variables for the C grid
260(1)
Discrete operators
261(1)
Conservation properties for the dynamics
262(3)
Conservation properties for the thermodynamics
265(1)
Discretization in time
265(1)
Robust diagnostic modelling
266(1)
Acceleration of convergence
267(2)
Surface boundary conditions
269(1)
Subgrid scale parameterisations
270(1)
Vertical mixing
270(3)
Convection
273(2)
Lateral mixing
275(2)
The global coupled system
277(11)
Ocean-only models
277(1)
Space or time?
277(1)
Oceanic observations
278(1)
Atmospheric forcing
278(1)
Sensitivity to parameterisation
278(3)
Coupled models
281(1)
General description of the problem
281(2)
Illustration of drift
283(1)
Flux correction
283(2)
Sensitivity
285(3)
The equatorial coupled system
288(20)
Oceanic equatorial waves
289(1)
Vertical eigenvectors
290(1)
Meridional normal modes
291(2)
Inertia-gravity and Rossby waves
293(2)
Mixed Rossby--gravity wave
295(1)
Equatorial Kelvin wave
295(1)
Equatorial waves and El Nino
296(1)
Response of forced simulations
297(1)
Coupled models
298(3)
Prediction
301(3)
Some new features to study El Nino
304(1)
Meridional coupling
304(1)
Barrier layer and freshwater flux
305(3)
Conclusion
308(7)
References
309(6)
Past Climatic Changes
315(62)
J.-C. Duplessy
Paleoclimatic and Paleoceanographic tools
319(18)
Introduction
319(1)
Transfer functions
320(1)
The Imbrie and Kipp (I&K) technique
320(2)
The Modern Analog Technique (MAT)
322(1)
Improving or validating transfer functions
322(4)
Stable isotope ratio variations
326(1)
Oxygen isotope fractionation during the water cycle
327(2)
Oxygen isotope fractionation during carbonate precipitation
329(3)
Isotope fractionation during the carbon cycle
332(2)
Dating
334(1)
Radiocarbon
334(2)
Uranium series disequilibria
336(1)
Longer time scales
336(1)
The climatic record of the Plio-Pleistocene and the evidence for the Astronomical Theory of paleoclimates
337(14)
Historcal introduction
337(2)
The Astronomical Theory of glaciations
339(3)
Extension of the climatic record over the last 6 million years
342(4)
The last climatic cycle
346(2)
The last glacial maximum
348(2)
The last climatic optimum
350(1)
Rapid variations within the climate system
351(26)
Introduction
351(1)
Evidence of rapid climatic change during the deglaciation
352(1)
Evidence of rapid climatic change during the glaciation
353(4)
Mechanisms of rapid climatic change under glacial conditions
357(2)
A case for the Younger Dryas
359(3)
Evidence of rapid climatic change during the Eemian
362(1)
Evidence of rapid climatic change during the Holocene
363(4)
Modeling of abrupt climatic changes and implications for future climates
367(2)
References
369(8)
Paleomyths I Have Known
377(72)
T.J. Crowley
Introduction
381(1)
General features of past climate change
381(4)
Some significant misconceptions about past climate change
385(2)
Discussion of the ``paleo-paradigms''
387(23)
``There is growing evidence that the tropics were about 5°C colder during the last glacial maximum''
387(8)
``North Atlantic deep water variations cause global temperature change''
395(3)
``Global warmth during the early Holocene and Last Interglacial was greater than present''
398(5)
``Deep water formation occurred in the subtropics during ice-free periods''
403(3)
``There is no evidence that low frequency variations in solar irradiance have occurred''
406(4)
Application to the problem of decadal--centennial scale variability
410(10)
Nature of observed changes
410(4)
Evaluating the relative contribution of different mechanisms to decadal--centennial climate change
414(2)
Variations of North Atlantic deep water
416(1)
Additional sources of oceanic variability
417(1)
Concluding remarks on natural variability: A challenge to modelers
418(2)
Concluding remarks
420(11)
References
422(9)
SPECIALIZED COURSES
Climate Variability of a Coupled Ocean--Atmosphere--Land Surface Model: Implication for the Detection of Global Warming
431(2)
S. Manabe
R.J. Stouffer
Introduction
433(1)
Numerical experiment
433(3)
Local variability
436(6)
Global variability
442(3)
Transient model response
445(1)
Concluding remarks
446(3)
References
447(2)
Variability of the Oceanic Thermohaline Circulation
449(78)
W.R. Holland
A. Capotondi
Introduction
453(1)
Experiments with a sector ocean driven by stochastic forcing
454(32)
The model
457(3)
Surface stochastic forcing
460(4)
Thermal boundary conditions
464(3)
The stochastically forced experiments
467(1)
Strong restoring cases
468(4)
Weak SST constraint
472(8)
Sensitivity to the spatial pattern
480(1)
Thermal stochastic forcing
481(1)
Effects of nonlinearities in the equation of state
482(3)
Discussion and conclusions for sector ocean model results
485(1)
Experiments with a regional North Atlantic ocean model driven by stochastic forcing
486(6)
A numerical experiment with the NCAR climate system model
492(30)
The ocean model and data sets used in the analyses
494(1)
Thermohaline circulation variability: year 30--year 299
495(10)
Period 1 (year 110--189)
505(7)
Period 2 (year 200--299)
512(9)
Discussion of CSM/North Atlantic results
521(1)
Discussion and conclusions
522(5)
References
523(4)
Modeling Extreme Climates of the Past 20,000 Years with General Circulation Models
527(40)
S. Joussaume
Introduction
531(2)
Methodology
533(4)
Simulating past climates
533(3)
Model--data comparisons
536(1)
The last glacial maximum
537(12)
PMIP experiments of the last glacial maximum
538(6)
Model--data comparisons
544(4)
Additional feedbacks
548(1)
Mid-Holocene climate
549(10)
PMIP simulations of the mid-Holocene
550(2)
Model--model comparisons
552(1)
Model--data comparisons
553(2)
Additional feedbacks
555(4)
Conclusions
559(8)
References
560(7)
Seminars by Participants 567

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