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Four model outputs with varying initial water i...

Four model outputs with varying initial water inventories denoted by blue shading. These...

Haskelle T. White-Gianella and Joshua Krissansen-Totton, The Planetary Science Journal 7 4

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The probability of reaching a final surface tem...

The probability of reaching a final surface temperature above 400 K for different initia...

Haskelle T. White-Gianella and Joshua Krissansen-Totton, The Planetary Science Journal 7 4

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Probability of the Monte Carlo model runs reach...

Probability of the Monte Carlo model runs reaching a final surface temperature of 400 K ...

Haskelle T. White-Gianella and Joshua Krissansen-Totton, The Planetary Science Journal 7 4

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Planetary surface temperatures after 4.5 Gyr of...

Planetary surface temperatures after 4.5 Gyr of model evolution as a function of the ini...

Haskelle T. White-Gianella and Joshua Krissansen-Totton, The Planetary Science Journal 7 4

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Precipitation estimated analytically for differ...

Precipitation estimated analytically for different surface temperatures assuming wind-dr...

Haskelle T. White-Gianella and Joshua Krissansen-Totton, The Planetary Science Journal 7 4

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Comparison of WHAK and MAC weathering formulati...

Comparison of WHAK and MAC weathering formulations with our geologic carbon cycle model ...

Haskelle T. White-Gianella and Joshua Krissansen-Totton, The Planetary Science Journal 7 4

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Schematic representation of the box model used ...

Schematic representation of the box model used in this study. Carbon fluxes are denoted ...

Haskelle T. White-Gianella and Joshua Krissansen-Totton, The Planetary Science Journal 7 4

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Similar to Figure 6, but additionally including...

Similar to Figure 6, but additionally including sensitivity tests where only the crust c...

Haskelle T. White-Gianella and Joshua Krissansen-Totton, The Planetary Science Journal 7 4

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Same as Figure A4 except with atmospheric escap...

Same as Figure A4 except with atmospheric escape processes excluded (α = 0.3). Neglectin...

Haskelle T. White-Gianella and Joshua Krissansen-Totton, The Planetary Science Journal 7 4

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The probability of reaching a final surface tem...

The probability of reaching a final surface temperature above 400 K for all unknown Mont...

Haskelle T. White-Gianella and Joshua Krissansen-Totton, The Planetary Science Journal 7 4

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Time distribution of when the model runs enter ...

Time distribution of when the model runs enter a runaway warming phase for Venus-like in...

Haskelle T. White-Gianella and Joshua Krissansen-Totton, The Planetary Science Journal 7 4

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Probability plot showing the effect of planetar...

Probability plot showing the effect of planetary hypsometry for Earth-like and Venus-lik...

Haskelle T. White-Gianella and Joshua Krissansen-Totton, The Planetary Science Journal 7 4

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Estimates of maximum crustal water inventory fr...

Estimates of maximum crustal water inventory from back-of-envelope calculations. The max...

Haskelle T. White-Gianella and Joshua Krissansen-Totton, The Planetary Science Journal 7 4

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Probability plot showing the effect of escape p...

Probability plot showing the effect of escape processes at Earth-like and Venus-like ins...

Haskelle T. White-Gianella and Joshua Krissansen-Totton, The Planetary Science Journal 7 4

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Same as Figure 3 except that escape processes a...

Same as Figure 3 except that escape processes are not included. Assumes Earth-like hypso...

Haskelle T. White-Gianella and Joshua Krissansen-Totton, The Planetary Science Journal 7 4

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Same as Figure 3 except water ingassing is surf...

Same as Figure 3 except water ingassing is surface dependent rather than mass dependent....

Haskelle T. White-Gianella and Joshua Krissansen-Totton, The Planetary Science Journal 7 4

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Probability plot showing the effect of escape p...

Probability plot showing the effect of escape processes at Earth-like and Venus-like ins...

Haskelle T. White-Gianella and Joshua Krissansen-Totton, The Planetary Science Journal 7 4

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Probability plot showing the effect of differen...

Probability plot showing the effect of different melt production regimes for Earth-like ...

Haskelle T. White-Gianella and Joshua Krissansen-Totton, The Planetary Science Journal 7 4

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Target ROIs (white polygons) pointed to by arro...

Target ROIs (white polygons) pointed to by arrows with the site names of D. De Rosa et a...

Ryodo Hemmi et al, The Planetary Science Journal 6 11

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Comparison of SP DTMs in the vicinity of CR1. E...

Comparison of SP DTMs in the vicinity of CR1. Each dataset is presented as a shaded-reli...

Ryodo Hemmi et al, The Planetary Science Journal 6 11

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Workflow overview. The pipeline has three stage...

Workflow overview. The pipeline has three stages. (1) Inputs and controls: build control...

Ryodo Hemmi et al, The Planetary Science Journal 6 11

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SfS DTMs gridded with 1 m pixel−1. They are col...

SfS DTMs gridded with 1 m pixel−1. They are color-coded by their elevations (50% opacity...

Ryodo Hemmi et al, The Planetary Science Journal 6 11

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The total population of valid overlapping pixel...

The total population of valid overlapping pixels among individual orthoimages. (a) CR1, ...

Ryodo Hemmi et al, The Planetary Science Journal 6 11

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Close-up views of the six target sites, represe...

Close-up views of the six target sites, represented by color-coded elevation of the 10 m...

Ryodo Hemmi et al, The Planetary Science Journal 6 11

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Close-ups of an NACL/NACR seam treated by two m...

Close-ups of an NACL/NACR seam treated by two methods. (a) Default ASP lronac2mosaic.py ...

Ryodo Hemmi et al, The Planetary Science Journal 6 11

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