Based on carbon dioxide concentrations at a location and wind speed, scientists trace particles back to their sources to identify whether the country is an emitter or a carbon sink, say Eurasian re

Though biodiversity and carbon storage have been linked in past forest research, a new study using Amazon, Congo and Borneo data found no consistent correlation.

NEW DELHI: If US President Donald Trump decides to withdraw from the Paris Agreement, it will dampen the spirit of global climate action as many countries not only look at America for support for t

Ecosystem carbon carrying capacity (CCC) is determined by prevailing climate and natural disturbance regimes, conditions that are projected to change significantly. The interaction of changing climate and its effects on disturbance regimes is expected to affect forest regeneration and growth, which may diminish forest carbon (C) stocks and uptake. We modeled landscape C dynamics over 590 years along the latitudinal gradient of the U.S. Sierra Nevada Mountains under climate and area burned by large wildfires projected by late 21st century.

In the Tibetan Plateau, climate change is increasing the carbon concentrations within the upper layers of permafrost soils, a study has shown.

Growth in terrestrial gross primary production (GPP)—the amount of carbon dioxide that is ‘fixed’ into organic material through the photosynthesis of land plants—may provide a negative feedback for climate change. It remains uncertain, however, to what extent biogeochemical processes can suppress global GPP growth. As a consequence, modelling estimates of terrestrial carbon storage, and of feedbacks between the carbon cycle and climate, remain poorly constrained.

This publication provides an overview to decision-makers and practitioners of the main scientific facts and information regarding the current knowledge and knowledge gaps on Soil Organic Carbon.

Question raised in Rajya Sabha on Eco-friendly approach for fulfillment of the Paris Climate Change Agreement, 20/03/2017. India ratified the Paris Agreement to the United Nations Framework Convention on Climate Change (UNFCCC) on 2nd October 2016.

The peatlands, which weren’t even known to exist as recently as five years ago, were revealed to cover 145,500 square kilometres (or more than 17,500 square miles), an area larger than England, and

The ocean is the largest sink for anthropogenic carbon dioxide (CO2), having absorbed roughly 40 per cent of CO2 emissions since the beginning of the industrial era. Recent data show that oceanic CO2 uptake rates have been growing over the past decade, reversing a trend of stagnant or declining carbon uptake during the 1990s. Here we show that ocean circulation variability is the primary driver of these changes in oceanic CO2 uptake over the past several decades.