39 research outputs found
Land Fraction Diversity on Earth-like Planets and Implications for their Habitability
A balanced ratio of ocean to land is believed to be essential for an
Earth-like biosphere and one may conjecture that plate-tectonics planets should
be similar in geological properties. After all, the volume of continental crust
evolves towards an equilibrium between production and erosion. If the interior
thermal states of Earth-sized exoplanets are similar to the Earth's, one might
expect a similar equilibrium between continental production and erosion to
establish and, hence, a similar land fraction. We will show that this
conjecture is not likely to be true. Positive feedback associated with the
coupled mantle water - continental crust cycle may rather lead to a manifold of
three possible planets, depending on their early history: a land planet, an
ocean planet and a balanced Earth-like planet. In addition, thermal blanketing
of the interior by the continents enhances the sensitivity of continental
growth to its history and, eventually, to initial conditions. Much of the
blanketing effect is however compensated by mantle depletion in radioactive
elements. A model of the long-term carbonate-silicate cycle shows the land and
the ocean planet to differ by about 5 K in average surface temperature. A
larger continental surface fraction results both in higher weathering rates and
enhanced outgassing, partly compensating each other. Still, the land planet is
expected to have a substantially dryer, colder and harsher climate possibly
with extended cold deserts in comparison with the ocean planet and with the
present-day Earth. Using a model of balancing water availability and nutrients
from continental crust weathering, we find the bioproductivity and the biomass
of both the land and ocean planet to be reduced by a third to half of Earth's.
The biosphere on these planets might not be substantial enough to produce a
supply of free oxygen
Bifurcation in the growth of continental crust
Is the present-day water-land ratio a necessary outcome of the evolution of
plate tectonic planets with a similar age, volume, mass, and total water
inventory as the Earth? This would be the case - largely independent of initial
conditions - if Earth's present-day continental volume were at a stable unique
equilibrium with strong self-regulating mechanisms of continental growth
steering the evolution to this state. In this paper, we question this
conjecture. Instead we suggest that positive feedbacks in the plate tectonics
model of continental production and erosion may dominate and show that such a
model can explain the history of continental growth.
We investigate the main mechanisms that contribute to the growth of the
volume of the continental crust. In particular, we analyze the effect of the
oceanic plate speed, depending on the area and thickness of thermally
insulating continents, on production and erosion mechanisms. Effects that cause
larger continental production rates for larger values of continental volume are
positive feedbacks. In contrast, negative feedbacks act to stabilize the
continental volume. They are provided by the increase of the rate of surface
erosion, subduction erosion, and crustal delamination with the continental
volume. We systematically analyze the strengths of positive and negative
feedback contributions to the growth of the continental crust. Although the
strengths of some feedbacks depend on poorly known parameters, we conclude that
a net predominance of positive feedbacks is plausible. We explore the effect of
the combined feedback strength on the feasibility of modeling the observed
small positive net continental growth rate over the past 2-3 billion years
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The Long-Term Evolution of the Atmosphere of Venus: Processes and Feedback Mechanisms: Interior-Exterior Exchanges
This work reviews the long-term evolution of the atmosphere of Venus, and modulation of its composition by interior/exterior cycling. The formation and evolution of Venus’s atmosphere, leading to contemporary surface conditions, remain hotly debated topics, and involve questions that tie into many disciplines. We explore these various inter-related mechanisms which shaped the evolution of the atmosphere, starting with the volatile sources and sinks. Going from the deep interior to the top of the atmosphere, we describe volcanic outgassing, surface-atmosphere interactions, and atmosphere escape. Furthermore, we address more complex aspects of the history of Venus, including the role of Late Accretion impacts, how magnetic field generation is tied into long-term evolution, and the implications of geochemical and geodynamical feedback cycles for atmospheric evolution. We highlight plausible end-member evolutionary pathways that Venus could have followed, from accretion to its present-day state, based on modeling and observations. In a first scenario, the planet was desiccated by atmospheric escape during the magma ocean phase. In a second scenario, Venus could have harbored surface liquid water for long periods of time, until its temperate climate was destabilized and it entered a runaway greenhouse phase. In a third scenario, Venus’s inefficient outgassing could have kept water inside the planet, where hydrogen was trapped in the core and the mantle was oxidized. We discuss existing evidence and future observations/missions required to refine our understanding of the planet’s history and of the complex feedback cycles between the interior, surface, and atmosphere that have been operating in the past, present or future of Venus
Planetary Exploration Horizon 2061 Report, Chapter 3: From science questions to Solar System exploration
This chapter of the Planetary Exploration Horizon 2061 Report reviews the way
the six key questions about planetary systems, from their origins to the way
they work and their habitability, identified in chapter 1, can be addressed by
means of solar system exploration, and how one can find partial answers to
these six questions by flying to the different provinces to the solar system:
terrestrial planets, giant planets, small bodies, and up to its interface with
the local interstellar medium. It derives from this analysis a synthetic
description of the most important space observations to be performed at the
different solar system objects by future planetary exploration missions. These
observation requirements illustrate the diversity of measurement techniques to
be used as well as the diversity of destinations where these observations must
be made. They constitute the base for the identification of the future
planetary missions we need to fly by 2061, which are described in chapter 4.
Q1- How well do we understand the diversity of planetary systems objects? Q2-
How well do we understand the diversity of planetary system architectures? Q3-
What are the origins and formation scenarios for planetary systems? Q4- How do
planetary systems work? Q5- Do planetary systems host potential habitats? Q6-
Where and how to search for life?Comment: 107 pages, 37 figures, Horizon 2061 is a science-driven, foresight
exercise, for future scientific investigation
Venus Evolution Through Time: Key Science Questions, Selected Mission Concepts and Future Investigations
In this work we discuss various selected mission concepts addressing Venus evolution through time. More specifically, we address investigations and payload instrument concepts supporting scientific goals and open questions presented in the companion articles of this volume. Also included are their related investigations (observations & modeling) and discussion of which measurements and future data products are needed to better constrain Venus’ atmosphere, climate, surface, interior and habitability evolution through time. A new fleet of Venus missions has been selected, and new mission concepts will continue to be considered for future selections. Missions under development include radar-equipped ESA-led EnVision M5 orbiter mission (European Space Agency 2021), NASA-JPL’s VERITAS orbiter mission (Smrekar et al. 2022a), NASA-GSFC’s DAVINCI entry probe/flyby mission (Garvin et al. 2022a). The data acquired with the VERITAS, DAVINCI, and EnVision from the end of this decade will fundamentally improve our understanding of the planet’s long term history, current activity and evolutionary path. We further describe future mission concepts and measurements beyond the current framework of selected missions, as well as the synergies between these mission concepts, ground-based and space-based observatories and facilities, laboratory measurements, and future algorithmic or modeling activities that pave the way for the development of a Venus program that extends into the 2040s (Wilson et al. 2022)
The Influence of the Biosphere on Continental Coverage and Mantle Hydration as Feedback Cycles in the Thermal Evolution of Earth
The Impact of Life on Climate Stabilization Over Different Timescales
Surface life has been argued to be crucial in keeping a planet habitable in the long term. Biologically enhanced weathering compensates for increasing solar luminosity, and temperature-dependent plant productivity weakens climate perturbations. Furthermore, a reduced calcification rate of marine organisms provides a negative feedback to rising atmospheric CO2. Here, I present a model of the long-term carbon cycle including biological enhancement of weathering and marine calcification. Climate oscillations of periods from thousands to millions of years arise from a simple model of mountain uplift and erosion. I systematically study the influence of the biologically driven feedbacks on damping these oscillations. For oscillations of periods 0.5 Myr. These findings are sensitive to the ratio of land to oceans, however. Furthermore, the mantle carbon degassing rate plays a role, since the temperature dependence of biological primary productivity may be smaller at higher temperatures. Altogether, life can be argued to stabilize the climate on timescales longer than some 100 kyr, while details depend on the geological state of the planet