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Global Temperature Change
by
Lea, David W.
, Ruedy, Reto
, Lo, Ken
, Hansen, James
, Sato, Makiko
, Medina-Elizade, Martin
in
Carbon dioxide emissions
/ Climate change
/ Climate models
/ Global climate
/ Global climate models
/ Global temperatures
/ Global warming
/ Greenhouse Effect
/ Greenhouse gases
/ Holocene
/ Ocean currents
/ Ocean temperature
/ Oceans
/ Oceans and Seas
/ Paleoclimate
/ Paleoclimatology
/ Physical Sciences
/ Sea level
/ Sea surface temperature
/ Seawater - analysis
/ Surface temperature
/ Temperature
/ Temperature gradients
/ Temperature scales
/ Time Factors
2006
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Global Temperature Change
by
Lea, David W.
, Ruedy, Reto
, Lo, Ken
, Hansen, James
, Sato, Makiko
, Medina-Elizade, Martin
in
Carbon dioxide emissions
/ Climate change
/ Climate models
/ Global climate
/ Global climate models
/ Global temperatures
/ Global warming
/ Greenhouse Effect
/ Greenhouse gases
/ Holocene
/ Ocean currents
/ Ocean temperature
/ Oceans
/ Oceans and Seas
/ Paleoclimate
/ Paleoclimatology
/ Physical Sciences
/ Sea level
/ Sea surface temperature
/ Seawater - analysis
/ Surface temperature
/ Temperature
/ Temperature gradients
/ Temperature scales
/ Time Factors
2006
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Do you wish to request the book?
Global Temperature Change
by
Lea, David W.
, Ruedy, Reto
, Lo, Ken
, Hansen, James
, Sato, Makiko
, Medina-Elizade, Martin
in
Carbon dioxide emissions
/ Climate change
/ Climate models
/ Global climate
/ Global climate models
/ Global temperatures
/ Global warming
/ Greenhouse Effect
/ Greenhouse gases
/ Holocene
/ Ocean currents
/ Ocean temperature
/ Oceans
/ Oceans and Seas
/ Paleoclimate
/ Paleoclimatology
/ Physical Sciences
/ Sea level
/ Sea surface temperature
/ Seawater - analysis
/ Surface temperature
/ Temperature
/ Temperature gradients
/ Temperature scales
/ Time Factors
2006
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Journal Article
Global Temperature Change
2006
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Overview
Global surface temperature has increased ≈0.2°C per decade in the past 30 years, similar to the warming rate predicted in the 1980s in initial global climate model simulations with transient greenhouse gas changes. Warming is larger in the Western Equatorial Pacific than in the Eastern Equatorial Pacific over the past century, and we suggest that the increased West-East temperature gradient may have increased the likelihood of strong El Niños, such as those of 1983 and 1998. Comparison of measured sea surface temperatures in the Western Pacific with paleoclimate data suggests that this critical ocean region, and probably the planet as a whole, is approximately as warm now as at the Holocene maximum and within 1°C of the maximum temperature of the past million years. We conclude that global warming of more than ≈1°C, relative to 2000, will constitute \"dangerous\" climate change as judged from likely effects on sea level and extermination of species.
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