Late Holocene methane rise caused by orbitally controlled increase in tropical sources. - Wikidata - wikimedia - TriplyDB

Late Holocene methane rise caused by orbitally controlled increase in tropical sources.

Late Holocene methane rise caused by orbitally controlled increase in tropical sources.

http://www.wikidata.org/entity/Q34162549

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Macroevolutionary consequences of profound climate change on niche evolution in marine molluscs over the past three million years Holocene variations in peatland methane cycling associated with the Asian summer monsoon system Enhanced chemistry-climate feedbacks in past greenhouse worlds Natural and anthropogenic variations in methane sources during the past two millennia.Tropical/Subtropical Peatland Development and Global CH4 during the Last Glaciation Understanding the glacial methane cycle.Glacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH4 ice core records.Constraints on the late holocene anthropogenic contribution to the atmospheric methane budget.A unifying conceptual model for the environmental responses of isoprene emissions from plants.Contrasting wetland CH4 emission responses to simulated glacial atmospheric CO2 in temperate bogs and fens.Global change: Methane and monsoons.Model evidence for a seasonal bias in Antarctic ice cores.Interglacials of the last 800,000 years Late Holocene climate: Natural or anthropogenic?The 8,000-year-old climate puzzle Glacial-interglacial water cycle, global monsoon and atmospheric methane changes Reconciling the changes in atmospheric methane sources and sinks between the Last Glacial Maximum and the pre-industrial era Lacustrine records of Holocene flood pulse dynamics in the Upper Paraguay River watershed (Pantanal wetlands, Brazil)Reduction of the temperature sensitivity of minerotrophic fen methane emissions by simulated glacial atmospheric carbon dioxide starvation Peatlands in the Earth’s 21st century climate system Collapse of the North American ice saddle 14,500 years ago caused widespread cooling and reduced ocean overturning circulation Flooding of the continental shelves as a contributor to deglacial CH4rise Controls on the tropospheric oxidizing capacity during an idealized Dansgaard-Oeschger event, and their implications for the rapid rises in atmospheric methane during the last glacial period

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P2860

Late Holocene methane rise caused by orbitally controlled increase in tropical sources.

http://www.wikidata.org/entity/Q34162549

description

2011 nî lūn-bûn

@nan

2011 թուականի Փետրուարին հրատարակուած գիտական յօդուած

@hyw

2011 թվականի փետրվարին հրատարակված գիտական հոդված

@hy

2011年の論文

@ja

2011年論文

@yue

2011年論文

@zh-hant

2011年論文

@zh-hk

2011年論文

@zh-mo

2011年論文

@zh-tw

2011年论文

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name

Late Holocene methane rise caused by orbitally controlled increase in tropical sources.

@ast

Late Holocene methane rise caused by orbitally controlled increase in tropical sources.

@en

Late Holocene methane rise caused by orbitally controlled increase in tropical sources.

@nl

type

label

Late Holocene methane rise caused by orbitally controlled increase in tropical sources.

@ast

Late Holocene methane rise caused by orbitally controlled increase in tropical sources.

@en

Late Holocene methane rise caused by orbitally controlled increase in tropical sources.

@nl

prefLabel

Late Holocene methane rise caused by orbitally controlled increase in tropical sources.

@ast

Late Holocene methane rise caused by orbitally controlled increase in tropical sources.

@en

Late Holocene methane rise caused by orbitally controlled increase in tropical sources.

@nl

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Late Holocene methane rise caused by orbitally controlled increase in tropical sources.

@en

P2093

Joy S Singarayer

http://www.w3.org/2001/XMLSchema#string

Paul J Valdes

http://www.w3.org/2001/XMLSchema#string

Sarah Nelson

http://www.w3.org/2001/XMLSchema#string

P2860

Atmospheric methane and nitrous oxide of the Late Pleistocene from Antarctic ice cores

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

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

Atmospheric CO2 concentrations over the last glacial termination.

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

Insolation values for the climate of the last 10 million years

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

The Anthropogenic Greenhouse Era Began Thousands of Years Ago

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

A note on the relationship between ice core methane concentrations and insolation

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82-85

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scholarly article

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10.1038/NATURE09739

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7332

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470

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Pierre Friedlingstein

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2011-02-01T00:00:00Z

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49809817

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21293375

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