Table 1 - Snow cover data requirements and priorities for system monitoring and climate change monitoring (Crane, 1993).
|
DATA CHARACTERISTICS |
DATA APPLICATIONS |
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|
Parameters |
Coverage |
Duration |
Frequency |
Global Climate Monitoring |
Earth System Models |
Process Models |
|
Snow cover extent |
H/R |
> 10 Years |
Daily/Weekly |
1 |
1 |
1 |
|
Snow water equivalent |
H/R |
> 10 Years |
Daily/Weekly |
2 |
1 |
1 |
|
Snow depth |
H/R |
> 10 Years |
Daily/Weekly |
1 |
2 |
2 |
|
Precipitation amount |
H/R |
> 10 Years |
Daily/Weekly |
2 |
1 |
1 |
|
Precipitation |
H/R |
> 10 Years |
Daily/Weekly |
2 |
1 |
1 |
|
Canopy (vegetation) |
H/R |
> 10 Years |
Daily/Weekly |
1 |
2 |
2 |
|
Albedo |
H/R |
> 10 Years |
Daily/Weekly |
2 |
1 |
2 |
|
Temperature |
H/R |
> 10 Years |
Daily/Weekly |
5 |
3 |
1 |
|
Melt (runoff) |
H/R |
> 10 Years |
Daily/Weekly |
5 |
3 |
1 |
H = Hemisphere
R = Regional
Ranking: 1 (high) to 5 (low).
Table 2 - Sea ice data requirements and priorities for system modelling and climate change monitoring (Crane, 1993).
|
DATA CHARACTERISTICS |
DATA APPLICATIONS |
|||||
|
Parameters |
Coverage |
Duration |
Frequency |
Global Climate Monitoring |
Earth System Models |
Process Models |
|
Concentration |
H/R |
10 Years |
Weekly/Monthly |
1 |
1 |
1 |
|
Thickness |
R/P |
10 Years |
Monthly/Seasonal |
1 |
1 |
1 |
|
Met obs |
R |
10 Years |
Daily |
1 |
1 |
1 |
|
Surface radiation |
R |
5 Years |
Hourly/Daily |
1 |
1 |
1 |
|
Albedo |
H/R |
10 Years |
Weekly |
2 |
1 |
1 |
|
Snow depth |
R/P |
5 Years |
Weekly |
2 |
2 |
1 |
|
Extent |
H/R |
10 Years |
Weekly/Monthly |
1 |
1 |
5 |
|
Leads/Polynyi |
R |
5 Years |
Weekly |
4 |
2 |
1 |
|
Ice temperature |
H/R |
5 Years |
Weekly/Monthly |
3 |
2 |
2 |
|
Ice type |
H/R |
10 Years |
Weekly/Monthly |
2 |
5 |
1 |
|
Ice motion |
H/R |
5 Years |
Weekly |
5 |
2 |
2 |
|
Melt ponds |
R |
5 Years |
Daily/Weekly |
3 |
4 |
2 |
|
Flow size distribution |
H/R |
5 Years |
Weekly |
5 |
5 |
2 |
|
Ridge statistics |
R |
5 Years |
Weekly |
5 |
5 |
2 |
H = Hemisphere
R = Regional
P = Point
Ranking: 1 (high) to 5 (low).
Table 3 - Ice sheet and glacier data requirements and priorities for system modelling and climate change monitoring (Crane, 1993).
|
DATA CHARACTERISTICS |
DATA APPLICATIONS |
|||||
|
Parameters |
Coverage |
Duration |
Frequency |
Global Climate Monitoring |
Earth System Models |
Process Models |
|
Snow accumulation |
GL/A |
> 10 Years |
Annually |
2 |
2 |
1 |
|
Ice extent |
G |
> 10 Years |
Annually |
1 |
5 |
5 |
|
Ice thickness |
G |
> 10 Years |
Annually |
1 |
5 |
1 |
|
Ice sheet DEM |
GL/A |
> 10 Years |
Decadally |
1 |
5 |
1 |
|
Ice velocity/surge activity |
G |
> 10 Years |
Annually |
2 |
5 |
2 |
|
Iceberg production |
GL/A |
> 10 Years |
Annually |
2 |
5 |
3 |
|
Mass balance |
G |
> 10 Years |
Annually |
1 |
5 |
5 |
|
Land ice fraction |
G.5 ×.5 |
> 10 Years |
Long-term mean |
5 |
3 |
5 |
GL = Greenland
A = Antarctica
G = Global
Ranking: 2 (high) to 5 (low).
Table 4 - Permafrost data requirements and priorities for modelling and change detection.
|
PARAMETERS |
APPLICATIONS |
||||
|
|
Process Understanding |
Engineering Design |
GCM Validation |
Change Detection |
Impact Evaluation |
|
GEOMETRY |
|||||
|
Permafrost extent |
M |
H |
H |
H |
M |
|
Permafrost thickness (shallow)* |
H |
H |
H |
H |
H |
|
Permafrost thickness (deep)* |
M |
M |
L |
H |
L |
|
Active layer thickness |
H |
H |
M |
H |
H |
|
Ground ice extent |
H |
H |
M |
M |
H |
|
Lateral/vertical displacement |
H |
H |
L |
H |
H |
|
THERMAL STATE |
|||||
|
Temperature (shallow*) |
H |
H |
H |
H |
H |
|
Temperature (deep*) |
M |
M |
M |
H |
L |
|
PROPERTIES (SOIL/ROCK) |
|||||
|
Moisture content (water/ice) |
H |
H |
M |
H |
H |
|
Bulk density |
H |
H |
H |
L |
L |
|
Texture |
H |
H |
L |
M |
M |
|
Chemistry (water/ice) |
M |
M |
L |
M |
M |
|
Trace gases |
H |
L |
H |
M |
M |
|
Site description: Location, geology, vegetation, geotechnical properties. |
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|
Metadata: Techniques, equipment, precision, post-processing, ownership, etc. |
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Notes: H, M, L = High, Moderate, and Low priority.
* For permafrost thickness and temperature, the demarcation between "shallow" and "deep" is taken as the local depth of zero annual amplitude.