With a pace of about twice the observed rate of global warming, the temperature on the
Qinghai‐Tibetan Plateau (Earth's 'third pole') has increased by 0.2° C per decade over the …

Contents Summary 35 I. Introduction 36 II. Tree CH4 fluxes 36 III. Tree emissions of soil‐
produced CH4 40 IV. Tree‐produced CH4 42 V. Trees in forest CH4 budgets 44 VI …

Global wetlands are believed to be climate sensitive, and are the largest natural emitters of
methane (CH 4). Increased wetland CH 4 emissions could act as a positive feedback to …

More than 250 plumes of gas bubbles have been discovered emanating from the seabed of
the West Spitsbergen continental margin, in a depth range of 150–400 m, at and above the …

The Intergovernmental Panel on Climate Change (IPCC) regularly publishes guidelines for
national greenhouse gas inventories and methane emission (CH4) from rice paddies has …

Terrestrial net CH 4 surface fluxes often represent the difference between much larger gross
production and consumption fluxes and depend on multiple physical, biological, and …

Methane (CH4) from aquatic ecosystems contributes to about half of total global CH4
emissions to the atmosphere. Until recently, aquatic biogenic CH4 production was …

Methane retrievals from the Scanning Imaging Absorption Spectrometer for Atmospheric
Chartography (SCIAMACHY) instrument onboard ENVISAT provide important information on …

High-accuracy continuous measurements of greenhouse gases (CO 2 and CH 4) during the
BARCA (Balanço Atmosférico Regional de Carbono na Amazônia) phase B campaign in …

Chemically active climate compounds are either primary compounds like methane (CH4),
removed by oxidation in the atmosphere, or secondary compounds like ozone (O3), sulfate …