The possibility of a reduced Atlantic thermohaline circulation in response to increases in
greenhouse-gas concentrations has been demonstrated in a number of simulations with …

The radiogenic isotope composition of dissolved trace metals in the ocean represents a set
of relatively new and not yet fully exploited tracers with a large potential for oceanographic …

• The sustained rate of increase over the past century in the combined radiative forcing from
the three well-mixed greenhouse gases carbon dioxide (CO2), methane (CH4), and nitrous …

A new earth system climate model of intermediate complexity has been developed and its
climatology compared to observations. The UVic Earth System Climate Model consists of a …

The climate sensitivity of the Community Climate System Model version 3 (CCSM3) is
studied for two past climate forcings, the Last Glacial Maximum (LGM) and the mid …

Abstract The Southern Ocean is widely recognized as a potential cause of the lower
atmospheric concentration of CO 2 during ice ages, but the mechanism is debated. Focusing …

The decay products of the long-lived radioactive systems are important tools for tracing
geological time and Earth processes. The main parent-daughter pairs used for studies in the …

The glacial cycles of the Pleistocene involve changes in the circulation of the deep ocean in
important ways. This review seeks to establish what were the robust patterns of deep‐sea …

Evidence from high-sedimentation-rate South Atlantic deep-sea cores indicates that global
and Southern Ocean carbon budget shifts preceded thermohaline circulation changes …

The radiogenic isotopic composition of both detrital and Fe–Mn fractions in marine
sediments can be used in paleoceanography to infer changes of bottom-water circulation …