Summary and Recommendations

  • The surface roughness and surface heat capacity can likely be improved in LANDUSE.TBL

    • Surface roughness can be decreased to 0.001 or 0.01. The former is more accurate, but I’m not sure how many orders of magnitude WRF can obtain from LANDUSE.TBL.

    • Specific heat capacity may be too high, but I’m concerned my calculations could be wrong.

  • Thermal inertia constant could also likely be improved, but I know my calculations are incorrect.

Other ice and snow sections from LANDUSE.TBL

Section

Season

Albedo
\((\%)\)

Suface Moisture Availability
\((*100\%)\)

Surface Emissivity
\((\%)\)

Surface Roughness

Thermal Inertia Constant

Snow Cover Effect

Surface Heat Capacity
\((J/(m^{3} K))\)

Category

OLD

Summer

55.

.95

.95

5.

5.

0.

9.0e25

Permanent Ice

OLD

Winter

70.

.95

.95

5.

5.

0.

9.0e25

Permanent Ice

USGS

Summer

55.

.95

.95

0.1

5.

0.

9.0e25

Snow or Ice

USGS

Winter

70.

.95

.95

0.1

5.

0.

9.0e25

Snow or Ice

MODIFIED_IGBP
_MODIS_NOAH

Summer

55.

.95

.95

0.1

5.

0

9.0e25

Snow or Ice

MODIFIED_IGBP
_MODIS_NOAH

Winter

70.

.95

.95

0.1

5.

0

9.0e25

Snow or Ice

SiB

Summer

55.

.95

.95

5.

5.

0.

9.0e25

Ice Cap and Glacier

SiB

Winter

70.

.95

.95

5.

5.

0.

9.0e25

Ice Cap and Glacier

LW12

All

70.

.95

.95

5.

5.

0.

9.0e25

Snow and Ice

MODIS

Summer

55.

.95

.95

1.

5.

0.

9.0e25

Snow and Ice

MODIS

Winter

55.

.95

.98

1.0

5.

0.

9.0e25

Snow and Ice

SSIB

Summer

55.

.95

.95

0.1

5.

0.

9.0e25

Snow or Ice

SSIB

Winter

70.

.95

.95

0.1

5.

0.

9.0e25

Snow or Ice

NLCD40

Summer

60.

.95

.95

1.2

5.

0.

9.0e25

Permanent Snow and Ice

NLCD40

Winter

60.

.95

.95

1.2

5.

0.

9.0e25

Permanent Snow and Ice

  • Albedos overall are lower than those observed at N-ICE

  • Soil moisture availability is 0.95 in all the simulations

  • Emissivity is higher in some situations, N-ICE simulations could potentially benefit from using the 0.98 instead of 0.95

  • Surface roughness is the lowest in the section used, but it is still higher than that calculated fro N-ICE

  • Thermal interia constant, snow cover effects, and the surface heat capacity are the same in all simualtions

    • If my calculations of the surface heat capacity are correct, simulations could likely be improved by lowering this value.

Values in VEGPARM.TBL

** Not used in the idealized simulations **

Section

Vegetation Fraction

Rooting Depth

Stomatal Resistance

Radiation Stress

Vapor Pressure Deficit Function Parameter

Soil Water Equivalent Snow Depth

Maximum Albedo Over Deep Snow

Minimum LAI

Maximum LAI

Minimum Emissivity

Maximum Emissivity

Minimum Albedo

Maximum Albedo

Minimum Roughness Length

Maximum Roughness Length

Category

USGS

0

1

999

999

999

0.02

82

0.01

0.01

0.95

0.95

0.55

0.70

0.001

0.001

Snow or Ice

MODIFIED_IGBP
_MODIS_NOAH

0

1

999

999

999

0.02

82

0.01

0.01

0.95

0.95

.55

.7

0.001

0.001

Snow and Ice

NLDC

0

1

999

999

999

0.02

82

0.01

0.01

0.95

0.95

0.55

0.70

0.001

0.001

Permanent Snow

NLDC

0

1

999

999

999

0.02

82

0.01

0.01

0.95

0.95

0.55

0.70

0.001

0.001

Perennial Ice/Snow

Section

Albedo

Roughness Length

LEMI*

PC*

Vegetation Factor

IFOR*

Stomatal Resistance

Radiation Stress

Vapor Pressure Deficit Function Parameter

Soil Water Equivalent Snow Depth

LAI

Maximum Albedo

Category

USGS-RUC

0.55

0.0024

0.98

0.00

0.00

9

999.

999.

999.

0.02

0.01

75

Snow or Ice

MODIS-RUC

0.55

0.011

0.98

0.00

0.00

9

999.

999.

999.

0.02

0.01

82

Snow and Ice

* I Don’t know what some of these are

  • The maximum albedo is higher here than in LANDUSE.TBL, closer to that seen at N-ICE and the value used in the simulations.

  • Roughness lengths are closer to what I’ve calculated for N-ICE

  • Emissivities are similar to those seen in LANDUSE.TBL

Values in SOILPARM.TBL

** Not used in the idealized simulation, for land-ice **

Section

B Parameter

Dry Soil Moisture Threshold

Soil Thermal Diffusivity/Conducticity Coefficient

Saturation Soil Moisture Content

Reference Soil Moisture

Saturation Soil Matric Potential

Saturation Soil Conductivity

Saturation Soil Diffusivity

Wilting Point Soil Moisture

Soil Quartz Content

STAS

4.26

0.028

-1.044

0.421

0.283

0.036

1.41E-5

0.514E-5

0.028

0.25

STAS-RUC

4.90

0.065

2.10

0.435

0.249

0.218

3.47E-5

0.514E-5

0.114

0.05

  • None of these should impact the ice surface

What do I recommend?

Section

Season

Albedo
\((\%)\)

Surface Moisture Availability
\((*100\%)\)

Surface Emissivity
\((\%)\)

Surface Roughness

Thermal Inertia Constant

Snow Cover Effect

Surface Heat Capacity
\((J/(m^{3} K))\)

NICE

Winter

86.

.95

.98

0.001

5.

0.

1.8e06

NICE

Summer

81.

.95

.98

0.001

5.

0.

1.8e06

  1. Increase albedo in both the winter and summer

  2. Increase surface emissivity from 0.95 to 0.98

  3. Decrease surface roughness from 0.1 to 0.001

  4. Decreased surface heat capacity and use a different value for winter and summer.