Transpiration (Kairouan, Tunisia - Dekadal) - WaPOR v2

The transpiration (T) data component (dekadal, in mm/day) is the actual transpiration of the vegetation canopy. The value of each pixel represents the average daily actual transpiration for that specific dekad.

Data publication: 2020-01-01

Supplemental Information:

No data value: 255

Unit: mm

Conversion factor: the pixel value in the downloaded data must be multiplied by 0.1

New dekadal data layers are released approximately 5 days after the end of a dekad. A higher quality version of the same data layer is uploaded after 6 dekads have passed. This final version of the dekadal dataset has a higher quality because gap filling and interpolation processes, where needed, have been based on more data observations.

Citation:

FAO 2018. WaPOR Database Methodology: Level 3. Remote Sensing for Water Productivity Technical Report: Methodology Series. Rome, FAO. 72 pages. Licence: CC BY-NC-SA 3.0 IGO

Contact points:

Metadata Contact: WaPOR

Resource Contact: WaPOR

Data lineage:

The calculation of the transpiration is based on the ETLook model described in Bastiaanssen et al. (2012). It uses the Penman-Monteith equation, adapted to remote sensing input data. The Penman-Monteith equation predicts the rate of total evaporation and transpiration using commonly measured meteorological data (solar radiation, air temperature, vapour content and wind speed). It has become the FAO standard for calculating the actual and reference evapotranspiration (see FAO Irrigation and Drainage paper 56, Allen et al. 1998).

The following data is used for calculating transpiration:

  • Daily: incoming solar radiation and weather data (temperature, humidity, wind speed and precipitation);

  • Dekadal: NDVI, surface albedo and soil moisture stress;

  • Seasonal: Land Cover;

  • Static: Digital Elevation Model.

Data component developed through collaboration with the FRAME Consortium. More information can be found at: http://www.fao.org/in-action/remote-sensing-for-water-productivity/en/

Resource constraints:

Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)

Online resources:

Transpiration (Kairouan, Tunisia - Dekadal)

Download data from WaPOR Website

Data and Resources

Metadata:

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dataIdentification
abstract
The transpiration (T) data component (dekadal, in mm/day) is the actual transpiration of the vegetation canopy. The value of each pixel represents the average daily actual transpiration for that specific dekad.
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utf8
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  • date
    2020-01-01
    dateType
    publication
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Version 2.0
otherCitationDetails
FAO 2018. WaPOR Database Methodology: Level 3. Remote Sensing for Water Productivity Technical Report: Methodology Series. Rome, FAO. 72 pages. Licence: CC BY-NC-SA 3.0 IGO
title
Transpiration (Kairouan, Tunisia - Dekadal) - WaPOR v2
descriptiveKeywords
  • keywords
    • Water
    • WaPOR
    • WaPOR_2
    • WaPOR_2_Subnational
    type
    theme
  • keywords
    • Dekadal
    type
    temporal
  • keywords
    • Africa
    • tunisia
    • kairouan
    type
    place
extent
  • temporal
    beginDate
    2015-01-01
  • geographic
    bbox
    east
    598300.0
    north
    3957980.0
    south
    3924700.0
    west
    558960.0
language
eng
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  • Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)
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asNeeded
spatialRepresentationType
  • grid
status
onGoing
supplementalInformation
No data value: 255 Unit: mm Conversion factor: the pixel value in the downloaded data must be multiplied by 0.1 New dekadal data layers are released approximately 5 days after the end of a dekad. A higher quality version of the same data layer is uploaded after 6 dekads have passed. This final version of the dekadal dataset has a higher quality because gap filling and interpolation processes, where needed, have been based on more data observations.
topicCategory
  • geoscientificInformation
  • climatologyMeteorologyAtmosphere
  • environment
  • farming
dataQualityInfo
lineage
statement
The calculation of the transpiration is based on the ETLook model described in Bastiaanssen et al. (2012). It uses the Penman-Monteith equation, adapted to remote sensing input data. The Penman-Monteith equation predicts the rate of total evaporation and transpiration using commonly measured meteorological data (solar radiation, air temperature, vapour content and wind speed). It has become the FAO standard for calculating the actual and reference evapotranspiration (see FAO Irrigation and Drainage paper 56, Allen et al. 1998). The following data is used for calculating transpiration: - Daily: incoming solar radiation and weather data (temperature, humidity, wind speed and precipitation); - Dekadal: NDVI, surface albedo and soil moisture stress; - Seasonal: Land Cover; - Static: Digital Elevation Model. Data component developed through collaboration with the FRAME Consortium. More information can be found at: http://www.fao.org/in-action/remote-sensing-for-water-productivity/en/
scope
series
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  • name
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    version
    8bit Unsigned Integer
fileIdentifier
25f431fd-3542-46fe-89bb-719c402f06da
language
eng
metadataStandardName
ISO 19115:2003/19139
metadataStandardVersion
1.0
referenceSystemIdentifier
EPSG:32632 - WGS 84 / UTM zone 32N
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  • cellGeometry
    area
    numberOfDimensions
    20m

Options:

validation
True

Type:

iso

Additional Info

Field Value
Source https://data.apps.fao.org/catalog/dataset/25f431fd-3542-46fe-89bb-719c402f06da
Last Updated December 20, 2023, 07:38 (UTC)
Created March 16, 2023, 11:01 (UTC)