Data for "Why are Mountaintops Cold? The Transition of Surface Lapse Rate on Dry Planets"
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Edited by Bowen Fan on 06/02/2023
0. This Dataset is for the paper “Why are Mountaintops Cold? The Transition of Surface Lapse Rate on Dry Planets”.
1. data_Fig1.mat: data for figure 1
lon: longitude
lat: latitude
Ts: surface temperature (unit in K) as a function of longitude, latitude, and case.
Z: surface elevation (unit in meter) as a function of longitude latitude, and case.
a: surface lapse rate (unit in %) for the cases in figure 1c
a1, a2, a3, a4, a5, a6: surface lapse rate (unit in %) for the cases in figure 1d
b1, b2, b3, b4, b5, b6, b7: surface lapse rate (unit in %) for the cases in figure 1e
2. data_Fig2.mat: data for figure 2
GSW: net solar heating (unit in W/m2) as a function of longitude, latitude, and case.
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.
3. data_Fig3.mat: data for figure 3
LWS_diff: the difference of surface emission between highland and lowland
LWA_diff: the difference of atmospheric emission between highland and lowland
SH_diff: the difference of sensible heat flux between highland and lowland
4. data_Fig4.mat: data for figure 4
a1, a2, a3, a4: surface lapse rate (unit in %) for the cases in figure 4a
c1, c2: surface lapse rate (unit in %) for the cases in figure 4b
5. data_FigS1.mat: data for supplementary figure 1
lon: longitude
lat: latitude
Ts: surface temperature (unit in K) as a function of longitude, latitude, and case.
Z: surface elevation (unit in meter) as a function of longitude latitude, and case.
a1, a2: surface lapse rate (unit in %) for the cases in figure S1c
6. data_FigS2.mat: data for supplementary figure 2
lon: longitude
lat: latitude
HGT: surface elevation (unit in meter) as a function of longitude latitude.
a1, a2: surface lapse rate (unit in %) for the cases in figure S2b
b1, b2: surface lapse rate (unit in %) for the cases in figure S2c
7. data_FigS3.mat: data for supplementary figure 3
lon: longitude
lat: latitude
T: near-surface air temperature (unit in K) as a function of longitude, latitude, and case.
Z: surface elevation (unit in meter) as a function of longitude latitude, and case.
U: near-surface zonal wind (unit in m/s) as a function of longitude, latitude, and case.
V: near-surface meridional wind (unit in m/s) as a function of longitude, latitude, and case.
8. data_FigS4.mat: data for supplementary figure 4
GSW: net solar heating (unit in W/m2) as a function of longitude, latitude, and case.
GLW: atmospheric heating (unit in W/m2) as a function of longitude, latitude, and case.
LWS: 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.
9. data_FigS3.mat: data for supplementary figure 5
Ts_local: surface temperature (unit in K) as a function of case and location (1 = highland, 2 = lowland).
Ps_local: surface pressure (unit in Pa) as a function of case and location.
T_local: atmospheric temperature profile as a function of height, case and location.
P_local: atmospheric pressure profile as a function of height, case and location.
T_ad: adiabatic atmospheric temperature profile as a function of height, case and location.
10. data_FigS6.mat: data for supplementary figure 6
10a. Cases with varied greenhouse forcing
SW_G LWA_G LWS_G SH_G: surface energy budgets from the GCM. The dimensions are location (1 for highland, 2 for lowland) and case.
LWA1_G, LWS1_G, SH1_G: surface energy budgets from the highland part of two-column model
LWA4_G, LWS4_G, SH4_G: surface energy budgets from the lowland part of two-column model
10b. Cases with varied surface pressure
SW_A LWA_A LWS_A SH_A: surface energy budgets from the GCM. The dimensions are location (1 for highland, 2 for lowland) and case.
LWA1_A, LWS1_A, SH1_A: surface energy budgets from the highland part of two-column model
LWA4_A, LWS4_A, SH4_A: surface energy budgets from the lowland part of two-column model
创建时间:
2023-10-05



