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Contribution of Working Group II to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change

TLDR
Drafting Authors: Neil Adger, Pramod Aggarwal, Shardul Agrawala, Joseph Alcamo, Abdelkader Allali, Oleg Anisimov, Nigel Arnell, Michel Boko, Osvaldo Canziani, Timothy Carter, Gino Casassa, Ulisses Confalonieri, Rex Victor Cruz, Edmundo de Alba Alcaraz, William Easterling, Christopher Field, Andreas Fischlin, Blair Fitzharris.
Abstract
Drafting Authors: Neil Adger, Pramod Aggarwal, Shardul Agrawala, Joseph Alcamo, Abdelkader Allali, Oleg Anisimov, Nigel Arnell, Michel Boko, Osvaldo Canziani, Timothy Carter, Gino Casassa, Ulisses Confalonieri, Rex Victor Cruz, Edmundo de Alba Alcaraz, William Easterling, Christopher Field, Andreas Fischlin, Blair Fitzharris, Carlos Gay García, Clair Hanson, Hideo Harasawa, Kevin Hennessy, Saleemul Huq, Roger Jones, Lucka Kajfež Bogataj, David Karoly, Richard Klein, Zbigniew Kundzewicz, Murari Lal, Rodel Lasco, Geoff Love, Xianfu Lu, Graciela Magrín, Luis José Mata, Roger McLean, Bettina Menne, Guy Midgley, Nobuo Mimura, Monirul Qader Mirza, José Moreno, Linda Mortsch, Isabelle Niang-Diop, Robert Nicholls, Béla Nováky, Leonard Nurse, Anthony Nyong, Michael Oppenheimer, Jean Palutikof, Martin Parry, Anand Patwardhan, Patricia Romero Lankao, Cynthia Rosenzweig, Stephen Schneider, Serguei Semenov, Joel Smith, John Stone, Jean-Pascal van Ypersele, David Vaughan, Coleen Vogel, Thomas Wilbanks, Poh Poh Wong, Shaohong Wu, Gary Yohe

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A statistical explanation of MaxEnt for ecologists

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Social Capital, Collective Action, and Adaptation to Climate Change

TL;DR: The authors argue that societies have inherent capacities to adapt to climate change, but these capacities are bound up in their ability to act collectively, and they argue that this capacity is limited by the nature of the agents of change, states, markets and civil society.
References
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Transient simulations of Holocene atmospheric carbon dioxide and terrestrial carbon since the Last Glacial Maximum

TL;DR: In this article, the Bern Carbon Cycle Climate (Bern CC) model is matched within a few ppm for the standard model setup, and results are broadly consistent with proxy data of atmospheric 13 CO2, mean ocean d 13 C, and pollen data, within their uncertainties.
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Causes of exceptional atmospheric circulation changes in the Southern Hemisphere

TL;DR: In this paper, the authors show that the observed trends in the Southern Hemisphere Annular Mode (SAM) are consistent with the combined effects of anthropogenic and natural forcings in GCM simulations.
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MSU Tropospheric Temperatures: Dataset Construction and Radiosonde Comparisons

TL;DR: In this paper, two deep-layer tropospheric temperature products, one for the lower troposphere (T2LT) and another for the mid-troposphere, are derived from the observations of channel 2 of the microwave sounding unit on National Oceanic and Atmospheric Administration (NOAA) polar-orbiting satellites.
Book

Temperature Trends in the Lower Atmosphere: Steps for Understanding and Reconciling Differences

TL;DR: This significant discrepancy no longer exists because errors in the satellite and radiosonde data have been identified and corrected as mentioned in this paper, and new data sets have also been developed that do not show such discrepancies.
Journal ArticleDOI

The Effects of Changing the Solar Constant on the Climate of a General Circulation Model

TL;DR: In this article, the authors evaluate the response of a simplified three-dimensional model climate to changes of the solar constant and find that the temperature of the model troposphere increases with increasing solar radiation, and the greatest increase occurs in the surface layer of higher latitudes due to the effects of the snow-cover feedback mechanism as well as the suppression of vertical mixing by a stable lower troposphere.
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