[HTML][HTML] Deglaciation of the Eurasian ice sheet complex
The Eurasian ice sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …
Taking climate model evaluation to the next level
Earth system models are complex and represent a large number of processes, resulting in a
persistent spread across climate projections for a given future scenario. Owing to different …
persistent spread across climate projections for a given future scenario. Owing to different …
[HTML][HTML] Recent third pole's rapid warming accompanies cryospheric melt and water cycle intensification and interactions between monsoon and environment …
Recent Third Pole’s Rapid Warming Accompanies Cryospheric Melt and Water Cycle
Intensification and Interactions between Monsoon and Environment: Multidisciplinary …
Intensification and Interactions between Monsoon and Environment: Multidisciplinary …
Historical greenhouse gas concentrations for climate modelling (CMIP6)
Atmospheric greenhouse gas (GHG) concentrations are at unprecedented, record-high
levels compared to the last 800 000 years. Those elevated GHG concentrations warm the …
levels compared to the last 800 000 years. Those elevated GHG concentrations warm the …
[HTML][HTML] The Polar Amplification Model Intercomparison Project (PAMIP) contribution to CMIP6: investigating the causes and consequences of polar amplification
Polar amplification–the phenomenon where external radiative forcing produces a larger
change in surface temperature at high latitudes than the global average–is a key aspect of …
change in surface temperature at high latitudes than the global average–is a key aspect of …
[HTML][HTML] Solar forcing for CMIP6 (v3. 2)
K Matthes, B Funke, ME Andersson… - Geoscientific Model …, 2017 - gmd.copernicus.org
This paper describes the recommended solar forcing dataset for CMIP6 and highlights
changes with respect to CMIP5. The solar forcing is provided for radiative properties, namely …
changes with respect to CMIP5. The solar forcing is provided for radiative properties, namely …
Northern Hemisphere vegetation change drives a Holocene thermal maximum
The Holocene thermal maximum, a period of global warmth evident in early to mid-Holocene
proxy reconstructions, is controversial. Most model simulations of the Holocene have not …
proxy reconstructions, is controversial. Most model simulations of the Holocene have not …
Last millennium Northern Hemisphere summer temperatures from tree rings: Part II, spatially resolved reconstructions
Climate field reconstructions from networks of tree-ring proxy data can be used to
characterize regional-scale climate changes, reveal spatial anomaly patterns associated …
characterize regional-scale climate changes, reveal spatial anomaly patterns associated …
[HTML][HTML] The PMIP4 contribution to CMIP6–Part 4: Scientific objectives and experimental design of the PMIP4-CMIP6 Last Glacial Maximum experiments and PMIP4 …
M Kageyama, S Albani, P Braconnot… - Geoscientific Model …, 2017 - gmd.copernicus.org
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 cloud feedback model intercomparison project (CFMIP) contribution to CMIP6
The primary objective of CFMIP is to inform future assessments of cloud feedbacks through
improved understanding of cloud–climate feedback mechanisms and better evaluation of …
improved understanding of cloud–climate feedback mechanisms and better evaluation of …