Climate state
The main climate state change is between periodical glacial and interglacial cycles in Earth history, studied from climate proxies. The climate system is responding to the current climate forcing and adjusts following climate sensitivity to reach a climate equilibrium, Earth's energy balance. Model simulations suggest that the current interglacial climate state will continue for at least another 100,000 years, due to CO2 emissions - including complete deglaciation of the Northern Hemisphere.
primaryTopic
Climate state
The main climate state change is between periodical glacial and interglacial cycles in Earth history, studied from climate proxies. The climate system is responding to the current climate forcing and adjusts following climate sensitivity to reach a climate equilibrium, Earth's energy balance. Model simulations suggest that the current interglacial climate state will continue for at least another 100,000 years, due to CO2 emissions - including complete deglaciation of the Northern Hemisphere.
has abstract
Der Klimazustand beschreibt de ...... wellenwerten ausgelöst werden.
@de
The main climate state change ...... on of the Northern Hemisphere.
@en
Link from a Wikipage to an external page
Wikipage page ID
40,552,929
Wikipage revision ID
740,269,265
type
comment
Der Klimazustand beschreibt de ...... e Klimaschwankungen entstehen.
@de
The main climate state change ...... on of the Northern Hemisphere.
@en
label
Climate state
@en
Klimazustand
@de
