S. A. Spall

TL;DR: Results from a fully coupled, three-dimensional carbon–climate model are presented, indicating that carbon-cycle feedbacks could significantly accelerate climate change over the twenty-first century.

TL;DR: In this article, the authors examined six coupled climate model simulations to determine the ocean biological response to climate warming between the beginning of the industrial revolution and 2050, and found that global warming leads to a contraction of the highly productive marginal sea ice biome by 42% in the Northern Hemisphere and 17% in Southern Hemisphere, and leads to an expansion of the low productivity permanently stratified subtropical gyre biome by 4.0% in both hemispheres.

TL;DR: In this paper, a GCM coupled climate-carbon cycle model is used to study the mechanisms involved in the relationship between ENSO and the carbon cycle, and the model simulates the observed temperature, precipitation, and CO 2 response of the climate to the El Nino Southern Oscillation (ENSO) cycle.

TL;DR: In this paper, a state-of-the-art fully coupled earth system model (HadCM3LC) was used to simulate the distribution of the last glacial maximum (LGM) for the continent of Africa.

TL;DR: In this paper, a new equation was developed whereby DMS is predicted from the product of chlorophyll (C, mg m −3 ), light ( J, mean daily shortwave, W m −2 ) and a nutrient term (Q, dimensionless) using a broken-stick regression.