Greenhouse Gases and Global Warming

The physical state of the climate system is determined by the interactions among the sun, atmosphere, biosphere (including humans), cryosphere (ice and snow), hydrosphere, and geosphere. Because of its complexity, a complete description of the climate system is beyond our capabilities. The use of observations and models can, however, increase our understanding of fundamental processes important in controlling the Earth’s mean climatic state.

[1]  John F. B. Mitchell,et al.  THE "GREENHOUSE" EFFECT AND CLIMATE CHANGE , 1989 .

[2]  Kevin P. Gallo,et al.  A new perspective on recent global warming: asymmetric trends of daily maximum and minimum temperature , 1993 .

[3]  K. Hasselmann,et al.  Transport and storage of CO2 in the ocean ——an inorganic ocean-circulation carbon cycle model , 1987 .

[4]  C. Lorius,et al.  Vostok ice core provides 160,000-year record of atmospheric CO2 , 1987, Nature.

[5]  G. Meehl,et al.  An example of fingerprint detection of greenhouse climate change , 1994 .

[6]  T. C. Johns,et al.  A search for human influences on the thermal structure of the atmosphere , 1995, Nature.

[7]  J. Imbrie,et al.  Ice Ages: Solving the Mystery , 1980 .

[8]  Veerabhadran Ramanathan,et al.  Climate modeling through radiative‐convective models , 1978 .

[9]  W. Broecker,et al.  What drives glacial cycles , 2013 .

[10]  K. Trenberth The use and abuse of climate models , 1997, Nature.

[11]  J. Daniel,et al.  On the evaluation of halocarbon radiative forcing and global warming potentials , 1995 .

[12]  Andrew A. Lacis,et al.  Sun and dust versus greenhouse gases: an assessment of their relative roles in global climate change , 1990, Nature.

[13]  Stephen H. Schneider,et al.  Detecting Climatic Change Signals: Are There Any "Fingerprints"? , 1994, Science.

[14]  Zong-ci Zhao,et al.  Climate models—evaluation , 2001 .

[15]  Jennifer A. Logan,et al.  Trends in the vertical distribution of ozone: An analysis of ozonesonde data , 1994 .

[16]  M. Khalil,et al.  Theory and development of a one dimensional time dependent radiative convective climate model , 1991 .

[17]  Donald J. Wuebbles,et al.  Primer on greenhouse gases , 1991 .

[18]  Jochen Harnisch,et al.  Tropospheric trends for CF4 and C2F6 since 1982 derived from SF6 dated stratospheric air , 1996 .

[19]  Michael J. Prather,et al.  Time scales in atmospheric chemistry: Theory, GWPs for CH4 and CO, and runaway growth , 1996 .

[20]  Richard L. Smith,et al.  Anthropogenic influence on the autocorrelation structure of hemispheric-mean temperatures , 1998, Science.

[21]  Douglas V. Hoyt,et al.  A discussion of plausible solar irradiance variations, 1700-1992 , 1993 .

[22]  Barry Saltzman,et al.  A Survey of Statistical-Dynamical Models of the Terrestrial Climate , 1978 .

[23]  J. Jouzel,et al.  Vostok ice core: a continuous isotope temperature record over the last climatic cycle (160,000 years) , 1987, Nature.

[24]  J. Lean,et al.  Estimating the Sun's radiative output during the Maunder Minimum , 1992 .

[25]  James J. Hack,et al.  Cloud feedback in atmospheric general circulation models: An update , 1996 .

[26]  K. Trenberth,et al.  Earth's annual global mean energy budget , 1997 .

[27]  J. Hansen,et al.  Global trends of measured surface air temperature , 1987 .

[28]  Normal modes and the transient response of the climate system , 1997 .

[29]  Robert E. Davis,et al.  The continuing search for an anthropogenic climate change signal: Limitations of correlation‐based approaches , 1997 .

[30]  J. Houghton Climate change 1994 : radiative forcing of climate change and an evaluation of the IPCC IS92 emission scenarios , 1995 .

[31]  V. Ramaswamy,et al.  Fingerprint of ozone depletion in the spatial and temporal pattern of recent lower-stratospheric cooling , 1996, Nature.

[32]  M. Khalil,et al.  Doubled CO2 experiments with the Global Change Research Center two-dimensional statistical dynamical climate model , 1995 .

[33]  P. Crutzen,et al.  A model study of atmospheric temperatures and the concentrations of ozone, hydroxyl, and some other photochemically active gases during the glacial, the pre-industrial holocene and the present , 1993 .

[34]  W. Washington,et al.  An Introduction to Three-Dimensional Climate Modeling , 1986 .

[35]  T. Wigley,et al.  Thermal expansion of sea water associated with global warming , 1987, Nature.

[36]  J. Harnisch,et al.  Effect of natural tetrafluoromethane , 1996, Nature.

[37]  S. Manabe,et al.  The Effects of Doubling the CO2 Concentration on the climate of a General Circulation Model , 1975 .

[38]  D. Hauglustaine,et al.  The importance of atmospheric chemistry in the calculation of radiative forcing on the climate system , 1994 .

[39]  P. Gilman,et al.  Solar rotation during the Maunder Minimum , 1976 .

[40]  An Estimation of the Climatic Effects of Stratospheric Ozone Losses during the 1980s. Appendix K , 1997 .

[41]  J. D. Tarpley,et al.  The recent climate record: What it can and cannot tell us , 1989 .

[42]  G. North Theory of Energy-Balance Climate Models. , 1975 .

[43]  P. Jones,et al.  Asymmetric trends of daily maximum and minimum temperature: Empirical evidence and possible causes , 1993 .

[44]  Michael E. Schlesinger,et al.  Detecting changes in global climate induced by greenhouse gases , 1987 .

[45]  N Oreskes,et al.  Verification, Validation, and Confirmation of Numerical Models in the Earth Sciences , 1994, Science.