served from IRI/LDEO Climate Data Library
Models SubC ESRL FIMr1p1 hindcast tas: 2-meter Mean Air Temperature data
2-meter Mean Air Temperature from Models SubC ESRL FIMr1p1 hindcast: FIMr1.1 Hindcast.Independent Variables (Grids)
- Lead (forecast_period)
- grid: /L (days) ordered (0.5 days) to (31.5 days) by 1.0 N= 32 pts :grid
- Ensemble Member (realization)
- grid: /M (ids) ordered (1) to (4) by 1.0 N= 4 pts :grid
- Start Time (forecast_reference_time)
- grid: /S (days since 1960-01-01) ordered (0000 6 Jan 1999) to (0000 28 Jun 2017) by 7.0 N= 965 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) periodic (0) to (1W) by 1.0 N= 360 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (90S) to (90N) by 1.0 N= 181 pts :grid
Other Info
- cell_method
- time: point
- cell_methods
- time: mean
- datatype
- realarraytype
- level_type
- 2 meters above ground
- pointwidth
- 0.0
- standard_name
- air_temperature
- units
- Kelvin_scale
- vartyp
- scalar
- standard units*
- degree_Kelvin above 0
Last updated: Wed, 10 Jan 2024 20:28:47 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| L | M | S | X | Y | |
 Models SubC ESRL FIMr1p1 hindcast tas[ X Y | L M S] | M | M | M | M | M |
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Filters
Here are some filters that are useful for manipulating data. There are actually many more available, but they have to be entered manually. See Ingrid Function Documentation for more information.- Monthly Climatology calculates a monthly climatology by averaging over all years.
- anomalies calculates the difference between the (above) monthly climatology and the original data.
- Integrate along X Y L M S
- Differentiate along X Y L M S
- Take differences along X Y L M S
RMS (root mean square with mean *not* removed) over X Y L M S | X Y X L X M X S Y L Y M Y S L M L S M S | X Y L X Y M X Y S X L M X L S X M S Y L M Y L S Y M S L M S | X Y L M X Y L S X Y M S X L M S Y L M S | X Y L M S |
RMSA (root mean square with mean removed) over X Y L M S | X Y X L X M X S Y L Y M Y S L M L S M S | X Y L X Y M X Y S X L M X L S X M S Y L M Y L S Y M S L M S | X Y L M X Y L S X Y M S X L M S Y L M S | X Y L M S |
Maximum over X Y L M S | X Y X L X M X S Y L Y M Y S L M L S M S | X Y L X Y M X Y S X L M X L S X M S Y L M Y L S Y M S L M S | X Y L M X Y L S X Y M S X L M S Y L M S | X Y L M S |
Minimum over X Y L M S | X Y X L X M X S Y L Y M Y S L M L S M S | X Y L X Y M X Y S X L M X L S X M S Y L M Y L S Y M S L M S | X Y L M X Y L S X Y M S X L M S Y L M S | X Y L M S |
Detrend (best-fit-line) over X Y L M S | X Y X L X M X S Y L Y M Y S L M L S M S | X Y L X Y M X Y S X L M X L S X M S Y L M Y L S Y M S L M S | X Y L M X Y L S X Y M S X L M S Y L M S | X Y L M S |
Note on units