An overview of interactions and feedbacks between ice sheets and the Earth system
Ice sheet response to forced changes—such as that from anthropogenic climate forcing—is
closely regulated by two‐way interactions with other components of the Earth system. These …
closely regulated by two‐way interactions with other components of the Earth system. These …
[HTML][HTML] The last interglacial climate: comparing direct and indirect impacts of insolation changes
RA Pedersen, PL Langen, BM Vinther - Climate Dynamics, 2017 - Springer
The last interglacial climate was influenced by substantial changes in the annual insolation
cycle that led to a warmer climate state with pronounced high northern latitude warming. We …
cycle that led to a warmer climate state with pronounced high northern latitude warming. We …
Response of Atlantic overturning to future warming in a coupled atmosphere‐ocean‐ice sheet model
Climate change can influence sea surface conditions and the melting rates of ice sheets;
resulting in decreased deep water formation rates and ultimately affecting the strength of the …
resulting in decreased deep water formation rates and ultimately affecting the strength of the …
Boreal winter stratospheric variability in EC-EARTH: High-Top versus Low-Top
FM Palmeiro, J García-Serrano, O Bellprat… - Climate Dynamics, 2020 - Springer
Abstract The European Consortium EC-EARTH climate model version 3.1 is used to assess
the role of a well-resolved stratosphere on stratospheric teleconnections in the Northern …
the role of a well-resolved stratosphere on stratospheric teleconnections in the Northern …
Arctic climate and its interaction with lower latitudes under different levels of anthropogenic warming in a global coupled climate model
Three quasi-equilibrium simulations using constant greenhouse gas forcing corresponding
to years 2000, 2015 and 2030 have been performed with the global coupled model EC …
to years 2000, 2015 and 2030 have been performed with the global coupled model EC …
Evolution of Ocean circulation in the North Atlantic Ocean during the Miocene: impact of the Greenland ice sheet and the Eastern Tethys Seaway
Abstract The Modern Ocean is characterized by the formation of deep‐water in the North
Atlantic Ocean (ie, NADW). This feature has been attributed to the modern geography, in …
Atlantic Ocean (ie, NADW). This feature has been attributed to the modern geography, in …
Impact of dust and temperature on primary productivity in Late Miocene oceans
Most of the primary productivity in the ocean comes from phytoplankton, and is impacted,
among other things, by the amount of nutrients available, as well as by temperature. The …
among other things, by the amount of nutrients available, as well as by temperature. The …
Expanding Greenland Ice Sheet Enhances Sensitivity of Plio‐Pleistocene Climate to Obliquity Forcing in the Kiel Climate Model
Proxy data suggest the onset of Northern Hemisphere glaciation during the Plio‐Pleistocene
transition from 3.2 to 2.5 Ma before present resulted in enhanced climate variability at the …
transition from 3.2 to 2.5 Ma before present resulted in enhanced climate variability at the …
Sea ice feedbacks influence the isotopic signature of Greenland ice sheet elevation changes: last interglacial HadCM3 simulations
Changes in the Greenland ice sheet (GIS) affect global sea level. Greenland stable water
isotope (δ 18 O) records from ice cores offer information on past changes in the surface of …
isotope (δ 18 O) records from ice cores offer information on past changes in the surface of …
Influences of Seaways, Atmospheric CO2 and Greenland Ice Sheet on the Pliocene Climate in the Kiel Climate Model
Z Song - 2017 - macau.uni-kiel.de
This thesis provides an improved understanding of the impacts of changes in the
atmospheric CO2-concentration, oceanic seaways, and Greenland ice sheet (GrIS) on the …
atmospheric CO2-concentration, oceanic seaways, and Greenland ice sheet (GrIS) on the …