Ice sheets matter for the global carbon cycle
JL Wadham, JR Hawkings, L Tarasov… - Nature …, 2019 - nature.com
The cycling of carbon on Earth exerts a fundamental influence upon the greenhouse gas
content of the atmosphere, and hence global climate over millennia. Until recently, ice …
content of the atmosphere, and hence global climate over millennia. Until recently, ice …
[HTML][HTML] The PMIP4 contribution to CMIP6–Part 1: Overview and over-arching analysis plan
This paper is the first of a series of four GMD papers on the PMIP4-CMIP6 experiments. Part
2 (Otto-Bliesner et al., 2017) gives details about the two PMIP4-CMIP6 interglacial …
2 (Otto-Bliesner et al., 2017) gives details about the two PMIP4-CMIP6 interglacial …
The PMIP4-CMIP6 Last Glacial Maximum experiments: preliminary results and comparison with the PMIP3-CMIP5 simulations
The Last Glacial Maximum (LGM,~ 21,000 years ago) has been a major focus for evaluating
how well state-of-the-art climate models simulate climate changes as large as those …
how well state-of-the-art climate models simulate climate changes as large as those …
A 156 kyr smoothed history of the atmospheric greenhouse gases CO2, CH4, and N2O and their radiative forcing
Continuous records of the atmospheric greenhouse gases (GHGs) CO 2, CH 4, and N 2 O
are necessary input data for transient climate simulations, and their associated radiative …
are necessary input data for transient climate simulations, and their associated radiative …
[HTML][HTML] The PMIP4 contribution to CMIP6–Part 4: Scientific objectives and experimental design of the PMIP4-CMIP6 Last Glacial Maximum experiments and PMIP4 …
The Last Glacial Maximum (LGM, 21 000 years ago) is one of the suite of paleoclimate
simulations included in the current phase of the Coupled Model Intercomparison Project …
simulations included in the current phase of the Coupled Model Intercomparison Project …
The PMIP4 contribution to CMIP6–Part 2: Two interglacials, scientific objective and experimental design for Holocene and Last Interglacial simulations
Two interglacial epochs are included in the suite of Paleoclimate Modeling Intercomparison
Project (PMIP4) simulations in the Coupled Model Intercomparison Project (CMIP6). The …
Project (PMIP4) simulations in the Coupled Model Intercomparison Project (CMIP6). The …
A reconciled solution of Meltwater Pulse 1A sources using sea-level fingerprinting
The most rapid global sea-level rise event of the last deglaciation, Meltwater Pulse 1A (MWP-
1A), occurred∼ 14,650 years ago. Considerable uncertainty regarding the sources of …
1A), occurred∼ 14,650 years ago. Considerable uncertainty regarding the sources of …
Greenland‐wide seasonal temperatures during the last deglaciation
The sensitivity of the Greenland ice sheet to climate forcing is of key importance in assessing
its contribution to past and future sea level rise. Surface mass loss occurs during summer …
its contribution to past and future sea level rise. Surface mass loss occurs during summer …
Compiled records of atmospheric CO2 concentrations and stable carbon isotopes to reconstruct climate and derive plant ecophysiological indices from tree rings
The stable carbon isotopic composition (δ 13 C) measured in tree rings is a standard proxy
for paleoclimate reconstructions and is increasingly being used as a paleophysiological …
for paleoclimate reconstructions and is increasingly being used as a paleophysiological …
Warm summers during the Younger Dryas cold reversal
Abstract The Younger Dryas (YD) cold reversal interrupts the warming climate of the
deglaciation with global climatic impacts. The sudden cooling is typically linked to an abrupt …
deglaciation with global climatic impacts. The sudden cooling is typically linked to an abrupt …