Add to ORKGUnderstanding how major modes of natural variability will respond to gradual mean state changes associated with anthropogenic warming is crucial to climate science (Corti et al. 1999). Coupled general circulation models (CGCMs
During the past 30 years--and in the near-term future--natural climate variability has been augmente...
International audienceTraditional general circulation models, or GCMs—that is, three-dimensional dyn...
A long-standing task in climate research has been to distinguish between anthropogenic climate chang...
Coupled general circulation models (CGCMs) integrate our knowledge about atmospheric and oceanic cir...
Coupled ocean-atmosphere general circulation models are used to predict future global changes, such ...
Although scientists now ac-cept global warming as in-controvertible, humans con-tinue to alter the c...
Global mean surface temperatures (GMST) warmed in the early 20th century, experienced a mid-century ...
The history of climate modeling begins with conceptual models, followed in the 19th century by mathe...
This article reviews some problems associated with the use of coupled atmosphere-ocean General Circu...
Since 1850 the global surface temperature (GST) has warmed by about 0.9 oC. The CMIP5 general circul...
During the whole history of the planet, astronomical factors (orbital and solar variability) have de...
We outline the familiar concept of a hierarchy of models for solving problems in climate dynamics. G...
Driven primarily by variations in the earth's axis wobble, tilt, and orbit eccentricity, our pl...
Global surface temperature records (e.g. HadCRUT4) since 1850 are characterized by climatic oscillat...
International audienceClimate variability, defined as changes in integral properties of the atmosphe...
During the past 30 years--and in the near-term future--natural climate variability has been augmente...
International audienceTraditional general circulation models, or GCMs—that is, three-dimensional dyn...
A long-standing task in climate research has been to distinguish between anthropogenic climate chang...
Coupled general circulation models (CGCMs) integrate our knowledge about atmospheric and oceanic cir...
Coupled ocean-atmosphere general circulation models are used to predict future global changes, such ...
Although scientists now ac-cept global warming as in-controvertible, humans con-tinue to alter the c...
Global mean surface temperatures (GMST) warmed in the early 20th century, experienced a mid-century ...
The history of climate modeling begins with conceptual models, followed in the 19th century by mathe...
This article reviews some problems associated with the use of coupled atmosphere-ocean General Circu...
Since 1850 the global surface temperature (GST) has warmed by about 0.9 oC. The CMIP5 general circul...
During the whole history of the planet, astronomical factors (orbital and solar variability) have de...
We outline the familiar concept of a hierarchy of models for solving problems in climate dynamics. G...
Driven primarily by variations in the earth's axis wobble, tilt, and orbit eccentricity, our pl...
Global surface temperature records (e.g. HadCRUT4) since 1850 are characterized by climatic oscillat...
International audienceClimate variability, defined as changes in integral properties of the atmosphe...
During the past 30 years--and in the near-term future--natural climate variability has been augmente...
International audienceTraditional general circulation models, or GCMs—that is, three-dimensional dyn...
A long-standing task in climate research has been to distinguish between anthropogenic climate chang...