served from IRI/LDEO Climate Data Library
Models SubC ECCC GEPS6 hindcast hfls: Surface Latent Heat Flux data
ECCC GEPS6 hindcast Surface Latent Heat Flux from Models SubC: Subseasonal Consortium (SubC).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 3 Jan 1998) to (0000 27 Dec 2017) by 1.0 N= 7299 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
- datatype
- realarraytype
- level
- surface
- level_type
- surface
- missing_value
- 9.99900026E20
- pointwidth
- 0.0
- short_name
- LHTFL_surface
- standard_name
- surface_upward_latent_heat_flux
- units
- W /m2
- standard units*
- kilogram second-3
Last updated: Tue, 03 Sep 2024 18:05:01 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 ECCC GEPS6 hindcast hfls[ 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