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pro vyhledávání: '"van Westen, Rene M."'
The Atlantic Meridional Overturning Circulation (AMOC) is recognized as a tipping element within the global climate system. Central to its tipping behavior is the salt-advection feedback mechanism, which has been extensively studied in box models and
Externí odkaz:
http://arxiv.org/abs/2410.03236
The Atlantic Meridional Overturning Circulation (AMOC) is a key component of the climate system and considered to be a tipping element. There is still a large uncertainty on the critical global warming level at which the AMOC will start to collapse.
Externí odkaz:
http://arxiv.org/abs/2407.19909
There is increasing concern that the Atlantic Meridional Overturning Circulation (AMOC) may collapse this century with a disrupting societal impact on large parts of the world. Preliminary estimates of the probability of such an AMOC collapse have so
Externí odkaz:
http://arxiv.org/abs/2406.11738
Recent simulations performed with the Community Earth System Model (CESM) have suggested a crucial role of sea-ice processes in AMOC hysteresis behaviour under varying surface freshwater forcing. Here, we further investigate this issue using addition
Externí odkaz:
http://arxiv.org/abs/2401.12615
The Atlantic Meridional Overturning Circulation (AMOC) is an important component of the global climate, known to be a tipping element, as it could collapse under global warming. The main objective of this study is to compute the probability that the
Externí odkaz:
http://arxiv.org/abs/2401.10800
Autor:
van Westen, René M., Dijkstra, Henk A.
We study hysteresis properties of the Atlantic Meridional Overturning Circulation (AMOC) under a slowly-varying North Atlantic (20$^{\circ}$N -- 50$^{\circ}$N) freshwater flux forcing in state-of-the-art Global Climate Model (GCM), the Community Eart
Externí odkaz:
http://arxiv.org/abs/2308.14098
Autor:
Dijkstra, Henk A., van Westen, Rene M.
It is known that global climate models (GCMs) have substantial biases in the surface freshwater flux which forces the ocean component of these models. Using numerical bifurcation analyses on a global ocean model, we study here the effect of a specifi
Externí odkaz:
http://arxiv.org/abs/2308.11751
One of the most prominent climate tipping elements is the Atlantic Meridional Overturning Circulation (AMOC), which can potentially collapse due to the input of fresh water in the North Atlantic. Although AMOC collapses have been induced in state-of-
Externí odkaz:
http://arxiv.org/abs/2308.01688
Publikováno v:
Nonlin. Processes Geophys. 30 (2023) 195-216
In recent years, several climate subsystems have been identified that may undergo a relatively rapid transition compared to the changes in their forcing. Such transitions are rare events in general, and simulating long-enough trajectories in order to
Externí odkaz:
http://arxiv.org/abs/2306.17049
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