Global temperature change

By J. Hansen, Makiko Sato, R. Ruedy, K. Lo, D. Lea, Martin Medina-Elizade. Proceedings of the National Academy of Sciences of the United States of America, 2006

2,096 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/65c0c2da273cce73e74382e29b9886eb9df53932

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Citations in the corpus

Hutchinson's duality: The once and future niche (2009, background): “2 illustrate an issue of intense current interest (27), as the global climate warms rapidly, already within 1 °C of the warmest it has been in at least the last million years (56).”
The impact of geoengineering aerosols on stratospheric temperature and ozone (2009, background): “Continuing anthropogenic greenhouse gas emissions might lead to dangerous future climate warming characterized by extreme weather events, shifting climatic zones, rising sea level and mass extinction (e.g. Hansen et al 2006, Solomon et al 2007).”
Interactions among Amazon land use, forests and climate: prospects for a near-term forest tipping point (2008, background): “Some climatologists believe that these anomalies will become more frequent as greenhouse gases accumulate further in the atmosphere (Trenberth & Hoar 1997; Timmermann et al. 1999; Hansen et al. 2006).”
Temperature effects on forest herbs assessed by warming and transplant experiments along a latitudinal gradient (2011, background): “Such temperature increases induce a latitudinal and altitudinal advance of the isotherms (Hansen et al., 2006), thereby moving the bioclimatic envelope of many species (recent review: Walther, 2010).”
Climate change and ocean acidification effects on seagrasses and marine macroalgae (2013, background): “1), mean global surface temperatures have increased by ~0.8 °C over the last century (Levitus et al., 2001; Hansen et al., 2006).”
Using temperature‐dependent changes in leaf scaling relationships to quantitatively account for thermal acclimation of respiration in a coupled global climate–vegetation model (2008, background): “The effects of acclimation may also vary through time in response to global warming (Cox et al., 2000; Hansen et al., 2006; IPCC, 2007).”
Variable shifts in spring and autumn migration phenology in North American songbirds associated with climate change (2009, background): “We expected to find some shifts in migration phenology because of the moderate increase in average temperatures across much of North and Middle America in recent decades (Easterling et al., 1997; Hansen et al., 2006).”
Time-series modeling and prediction of global monthly absolute temperature for environmental decision making (2013, methodology): “This is notable because global temperature reached the record warmth in 2005 without receiving a boost from an El Niño event (Hansen et al., 2006), meaning that global temperature could become higher than predicted if it is coincident with a strong El Niño.”
Public perceptions of energy consumption and savings (2010, background): “A CO2 emissions are contributing to global climate change (1) and could negatively impact our way of life if serious action is further delayed.”
Economic aspects of global warming in a post-Copenhagen environment (2010, background): “These include CO2 emissions from land-use changes, non-CO2 GHGs, and sulfate aerosols (18, 19).”
The impact of global warming on plant diseases and insect vectors in Sweden (2010, background): “It is clear that the climate is changing and the temperature is projected to undergo a relatively high rise in Sweden compared to the overall global mean change (Hansen et al. 2006; SMHI 2010; Leijonhufvud et al. 2010).”
Climate change and Australian marine life (2007, background): “The 1990s were the warmest decade globally of the past century; and the present decade may be warmest yet (Hansen et al. 2006).”