Late Holocene methane rise caused by orbitally controlled increase in tropical sources (Q34162549)

31 July 2017

title

Late Holocene methane rise caused by orbitally controlled increase in tropical sources (English)

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31 July 2017

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5

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31 July 2017

Pierre Friedlingstein

series ordinal

3

object named as

Pierre Friedlingstein

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Paul J. Valdes

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2

object named as

Paul J Valdes

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31 July 2017

Joy S Singarayer

1

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31 July 2017

Sarah Nelson

series ordinal

4

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31 July 2017

language of work or name

English

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publication date

1 February 2011

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31 July 2017

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31 July 2017

volume

470

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31 July 2017

issue

7332

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31 July 2017

page(s)

82-85

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The Anthropogenic Greenhouse Era Began Thousands of Years Ago

31 July 2017

cites work

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Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 years

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Changing boreal methane sources and constant biomass burning during the last termination

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Monsoon Climate of the Early Holocene: Climate Experiment with the Earth's Orbital Parameters for 9000 Years Ago.

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The impact of new physical parametrizations in the Hadley Centre climate model: HadAM3

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GLOBAL GLACIAL ISOSTASY AND THE SURFACE OF THE ICE-AGE EARTH: The ICE-5G (VM2) Model and GRACE

21 January 2018

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Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica

21 January 2018

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Insolation values for the climate of the last 10 million years

21 January 2018

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A global model of natural volatile organic compound emissions

21 January 2018

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Mid-Holocene and Last Glacial Maximum African monsoon changes as simulated within the Paleoclimate Modelling Intercomparison Project

21 January 2018

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Atmospheric CO2 concentrations over the last glacial termination

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Early rice farming and anomalous methane trends

21 January 2018

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Observations and modeling of biomass and soil organic matter dynamics for the grassland biome worldwide

21 January 2018

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The ice age methane budget

21 January 2018

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The effects of glacial atmospheric CO2 concentrations and climate on isoprene emissions by vascular plants

21 January 2018

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The simulation of SST, sea ice extents and ocean heat transports in a version of the Hadley Centre coupled model without flux adjustments

21 January 2018

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Changes in the atmospheric CH4gradient between Greenland and Antarctica during the Holocene

21 January 2018

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Variations in atmospheric methane concentration during the Holocene epoch

21 January 2018

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Evaluation of the terrestrial carbon cycle, future plant geography and climate-carbon cycle feedbacks using five Dynamic Global Vegetation Models (DGVMs)

21 January 2018

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Role of convection in determining the budget of odd hydrogen in the upper troposphere

21 January 2018

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The case for human causes of increased atmospheric CH4 over the last 5000 years

21 January 2018

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Responses of global plant diversity capacity to changes in carbon dioxide concentration and climate

21 January 2018

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https://pubmed.ncbi.nlm.nih.gov/21293375

12 December 2020

inferred from PubMed ID database lookup

Climatic changes of the last 18,000 years: observations and model simulations

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https://pubmed.ncbi.nlm.nih.gov/21293375

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Why are estimates of global terrestrial isoprene emissions so similar (and why is this not so for monoterpenes)?

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7 January 2021

Results of PMIP2 coupled simulations of the Mid-Holocene and Last Glacial Maximum – Part 1: experiments and large-scale features

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7 January 2021

Results of PMIP2 coupled simulations of the Mid-Holocene and Last Glacial Maximum – Part 2: feedbacks with emphasis on the location of the ITCZ and mid- and high latitudes heat budget

1 reference

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7 January 2021

CO2fertilization in temperate FACE experiments not representative of boreal and tropical forests

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https://api.crossref.org/works/10.1038%2FNATURE09739

7 January 2021

CO2inhibition of global terrestrial isoprene emissions: Potential implications for atmospheric chemistry

1 reference

https://api.crossref.org/works/10.1038%2FNATURE09739

7 January 2021

Identifiers

DOI

10.1038/NATURE09739

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Dimensions Publication ID

31 July 2017

1043197574

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