Unexpected Changes to the Global Methane Budget over the Past 2000 Years
暂无分享,去创建一个
D. Etheridge | C. Trudinger | R. Langenfelds | J. Miller | D. Lowe | T. V. van Ommen | J. White | J. White | K. Lassey | T. Ommen | D. Ferretti | C. M. Meure | M. Dreier | John B. Miller
[1] K. Holmgren,et al. Highly variable Northern Hemisphere temperatures reconstructed from low- and high-resolution proxy data , 2005, Nature.
[2] Giuseppe Etiope,et al. New Directions: GEM—Geologic Emissions of Methane, the missing source in the atmospheric methane budget☆ , 2004 .
[3] W. Ruddiman,et al. The Anthropogenic Greenhouse Era Began Thousands of Years Ago , 2003 .
[4] D. Hallett,et al. A 1000-year record of forest fire, drought and lake-level change in southeastern British Columbia, Canada , 2003 .
[5] K. Gajewski,et al. Holocene biomass burning and global dynamics of the carbon cycle. , 2002, Chemosphere.
[6] J. Lelieveld,et al. A 1°×1° resolution data set of historical anthropogenic trace gas emissions for the period 1890–1990 , 2001 .
[7] M. Andreae,et al. Emission of trace gases and aerosols from biomass burning , 2001 .
[8] W. Sturges,et al. Changes in the global atmospheric methane budget over the last decades inferred from13C and D isotopic analysis of Antarctic firn air , 2001 .
[9] Georg Guggenberger,et al. The 'Terra Preta' phenomenon: a model for sustainable agriculture in the humid tropics , 2001, Naturwissenschaften.
[10] J. Lelieveld,et al. Simulation of preindustrial atmospheric methane to constrain the global source strength of natural wetlands , 2000 .
[11] M. Manning,et al. The trend in atmospheric methane δ13C and implications for isotopic constraints on the global methane budget , 2000 .
[12] Dirk Verschuren,et al. Rainfall and drought in equatorial east Africa during the past 1,100 years , 2000, Nature.
[13] D. Etheridge,et al. A history of δ13C in atmospheric CH4 from the Cape Grim Air Archive and Antarctic firn air , 1999 .
[14] J. Jouzel,et al. Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica , 1999, Nature.
[15] Yuhang Wang,et al. Anthropogenic forcing on tropospheric ozone and OH since preindustrial times , 1998 .
[16] D. Etheridge,et al. Atmospheric methane between 1000 A.D. and present: Evidence of anthropogenic emissions and climatic variability , 1998 .
[17] G. Ren. Pollen evidence for increased summer rainfall in the medieval warm period at Maili, northeast China , 1998 .
[18] M. Legrand,et al. High northern latitude forest fires and vegetation emissions over the last millennium inferred from the chemistry of a central Greenland ice core , 1998 .
[19] M. Manning,et al. The 1991–1992 atmospheric methane anomaly: Southern hemisphere 13C decrease and growth rate fluctuations , 1997 .
[20] M. Anderson. Prehistoric anthropogenic wildland burning by hunter-gatherer societies in the temperate regions: A net source, sink, or neutral to the global carbon budget? , 1994 .
[21] S. Subak. Methane from the House of Tudor and the Ming Dynasty: Anthropogenic emissions in the sixteenth century , 1994 .
[22] D. Woodcock,et al. The burning of the New World: the extent and significance of broadcast burning by early humans. , 1994, Chemosphere.
[23] T. Swetnam. Fire History and Climate Change in Giant Sequoia Groves , 1993, Science.
[24] C. M. Stevens,et al. The Isotopic Composition of Methane in Polar Ice Cores , 1988, Science.
[25] M. Khalil,et al. Atmospheric methane in the recent and ancient atmospheres Concentrations, trends, and interhemispheric gradient , 1984 .
[26] J. Houdaille. Native (the) population of the Americas in 1492 , 1978 .