Two drastically different climate states on an Earth-like terra-planet
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Published:2018-06-07
Issue:2
Volume:9
Page:739-756
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ISSN:2190-4987
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Container-title:Earth System Dynamics
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language:en
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Short-container-title:Earth Syst. Dynam.
Author:
Kalidindi Sirisha, Reick Christian H., Raddatz Thomas, Claussen MartinORCID
Abstract
Abstract. We study an Earth-like terra-planet (water-limited terrestrial planet) with
an overland recycling mechanism bringing fresh water back from the high
latitudes to the low latitudes. By performing model simulations for such a
planet we find two drastically different climate states for the same set of
boundary conditions and parameter values: a cold and wet (CW) state with
dominant low-latitude precipitation and a hot and dry (HD) state with only
high-latitude precipitation. We notice that for perpetual equinox conditions,
both climate states are stable below a certain threshold value of background
soil albedo while above the threshold only the CW state is stable. Starting
from the HD state and increasing background soil albedo above the threshold
causes an abrupt shift from the HD state to the CW state resulting in a
sudden cooling of about 35 ∘C globally, which is of the order of the
temperature difference between present day and the Snowball Earth state.
When albedo starting from the CW state is reduced down to zero the
terra-planet does not shift back to the HD state (no closed hysteresis). This
is due to the high cloud cover in the CW state hiding the surface from solar
irradiation so that surface albedo has only a minor effect on the top of the
atmosphere radiation balance. Additional simulations with present-day Earth's
obliquity all lead to the CW state, suggesting a similar abrupt transition
from the HD state to the CW state when increasing obliquity from zero. Our
study also has implications for the habitability of Earth-like terra-planets.
At the inner edge of the habitable zone, the higher cloud cover in the CW
state cools the planet and may prevent the onset of a runaway greenhouse
state. At the outer edge, the resupply of water at low latitudes stabilizes
the greenhouse effect and keeps the planet in the HD state and may prevent
water from getting trapped at high latitudes in frozen form. Overall, the
existence of bistability in the presence of an overland recycling mechanism
hints at the possibility of a wider habitable zone for Earth-like
terra-planets at low obliquities.
Publisher
Copernicus GmbH
Subject
General Earth and Planetary Sciences
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