Edited by Bowen Fan on 09/29/2022

0.	This Dataset is for the paper “Why are Mountaintops Cold? The Decorrelation of Surface Temperature and Elevation Due to the Greenhouse Effect Weakening on Early Mars”. The main.mat file includes data necessary to produce figures in the main text, while SI.mat includes matrixes in the supporting information.

1.	Main.mat:
1.1	Figure 1
Lon: longitude
Lat: latitude
Ts: surface temperature (unit in K) as a function of longitude, latitude, and case. The 4 cases are "CO2 scheme, Ps = 3 bar, modern Mars topography", "CO2 scheme, Ps = 0.01 bar, modern Mars topography", "gray gas scheme, Ps = 1 bar, tau = 10, ideal topography", and "gray gas scheme, Ps = 1 bar, tau = 0.01, ideal topography", respectively.
Z: surface elevation (unit in meter) as a function of longitude latitude, and case. 
Gamma1: surface lapse rate (unit in %) for the "CO2 scheme, modern Mars topography" cases, from Ps = 0.01 bar to Ps = 3 bar 
Gamma2: surface lapse rate for the "CO2 scheme, ideal topography" cases, from Ps = 0.01 bar to Ps = 3 bar
Gamma: surface lapse rate as a function of Ps and tau for "gray scheme, ideal topography" cases.

1.2	Figure 2
GSW: net solar heating (unit in W/m2) as a function of longitude, latitude, and case. The 7 cases are "CO2 scheme, Ps = 1 bar", "CO2 scheme, Ps = 0.1 bar", "CO2 scheme, Ps = 0.01 bar", "gray gas scheme, Ps = 1 bar, tau = 10", "gray gas scheme, Ps = 1 bar, tau = 1", "gray gas scheme, Ps = 1 bar, tau = 0.1", and "gray gas scheme, Ps = 1 bar, tau = 0.01", respectively.
GLW: atmospheric heating (unit in W/m2) as a function of longitude, latitude, and case.
TSK: surface emission (unit in W/m2) as a function of longitude, latitude, and case.
HFX: sensible cooling (unit in W/m2) as a function of longitude, latitude, and case.

1.3	Figure 3
Press: equatorial pressure matrix as a function of case and pressure (unit in hPa) for Fig. 3a1, 3b1, 3c1, 3d1. The 4 cases are "3-bar CO2", "0.01-bar CO2", "1-bar gray gas with tau = 0.01", and "1-bar gray gas with tau = 10", respectively.
Temp: equatorial atmospheric temperature matrix as a function of case and temperature (unit in K).
Ps_local: local surface pressure (unit in hPa) as a function of case and location. The 1st location is the equatorial highland in the ideal topography, the 2nd location is the equatorial lowland in the ideal topography.
Ts_local: local surface temperature (unit in K) as a function of case and location.
P_local: local atmospheric pressure (unit in hPa) as a function of level, case, and location. 
T_local: local atmospheric temperature (unit in K) as a function of level, case, and location.
T_ad: local atmospheric temperature (unit in K) as a function of level, case, and location if the air is adiabatic starting from the 1st (near-surface) atmospheric level/


2.	Supporting Information
2.1	Table S1
Lon: longitude
Lat: latitude
HGT: surface elevation (unit in meter) as a function of longitude latitude, and case. The 2 cases are "ideal narrow topography" and "ideal wide topography".
Gamma1: surface lapse rate (unit in %) for the "CO2 scheme, modern Mars topography" cases, from Ps = 0.01 bar to Ps = 3 bar 
Gamma2: surface lapse rate for the "CO2 scheme, ideal Gaussian topography" cases, from Ps = 0.01 bar to Ps = 3 bar 
Gamma3: surface lapse rate for the "CO2 scheme, ideal narrow topography" cases, from Ps = 0.01 bar to Ps = 3 bar 
Gamma4: surface lapse rate for the "CO2 scheme, ideal wide topography" cases, from Ps = 0.01 bar to Ps = 3 bar 
GSW: net solar heating (unit in W/m2) as a function of longitude, latitude, and case. The 6 cases are "CO2 scheme, Ps = 1 bar, narrow topography", "CO2 scheme, Ps = 0.1 bar, narrow topography", "CO2 scheme, Ps = 0.01 bar, narrow topography", "CO2 scheme, Ps = 1 bar, wide topography", "CO2 scheme, Ps = 0.1 bar, wide topography", and "CO2 scheme, Ps = 0.01 bar, wide topography", respectively.
GLW: atmospheric heating (unit in W/m2) as a function of longitude, latitude, and case.
TSK: surface emission (unit in W/m2) as a function of longitude, latitude, and case.
HFX: sensible cooling (unit in W/m2) as a function of longitude, latitude, and case.
