Integrated Climate Data Center

MODIS NDVI

MODIS NDVI for March 2010.

Access

UNRESTRICTED

This data set is only available for a restricted user group, please contact us if you want to access these data.

RESTRICTED only accessable in ZMAW net or via CliSAP login  What does that mean?

View data via LAS

Data access via OPeNDAP

Data access via file system /data/icdc/land/modis_vegetationindex

 

Description

This data set comprises the Normalized Differential Vegetation Index (NDVI) and the Enhanced Vegetation Index (EVI) together with uncertainty estimates and quality flags. Both indices are based on the difference: reflectance observed in the near-infrared (NIR) portion of the electromagnetic spectrum minus reflectance observed in the red portion of the electromagnetic spectrum. Areas with photosynthetically active vegetation absorb much more radiation in the red portion of the electromagnetic spectrum than areas without any or with photosynthetically inactive vegetation. This is due to the pigments in the leaves, needles, etc. In contrast, absorption of NIR radiation is low for both surface types. However, the amount of NIR radiation transmitted and/or scattered is a function of the surface type / roughness. Therefore, the difference of the reflectances is small for areas without any or with photosynthetically inactive vegetation and high for areas with photosynthetically active vegetation. Note that in areas with a lot of vegetation the dependence of the NIR-radiation scattering and/or transmission on the surface type / roughness helps to overcome saturation effects in the red portion of the electromagnetic spectrum and therefore allows a better separation of high NDVI values.

The impact of clouds, aerosols, sensor noise (and other error sources not mentioned here explicitly) is mitigated using radiative transfer modeling on the one hand. On the other hand these impacts are mitigated by normalizing the above-mentioned difference with the sum of the used reflectances (NDVI) or with these reflectances, the reflectance in the blue portion of the electromagnetic spectrum and additional factors (EVI). For more details we recommend to look into the User's Guide.

The data set offered here has monthly temporal resolution and allows to monitor the seasonal cycle of vegetation development.

 

 

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Parameters

Name Unit
NDVI --
NDVI standard deviation --
EVI --
EVI standard deviation --
quality flag (general) --
quality flag (detailed) --
quality flag spatial coverage --
quality flag aerosol model --
   

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Coverage, spatial and temporal resolution

Period and temporal resolution:

  • 02/2000 - 12/2012
  • Monthly

Coverage and spatial resolution:

 

  • Global
  • Spatial resolution: 0.05° x 0.05° (about 5600 m, Climate Modeling Grid)
  • Geographical longitude: 179.975°W to 179.975°E
  • Geographical latitude: 89.975°S to 89.975°N
  • Dimension: 3600 rows x 7200 columns
  • Altitude: follows topography

Format

  • NetCDF

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Data quality

This is version 5 of this MODIS data set. Both, NDVI and EVI have been validated in a number of field campaigns and validation studies. The data set with monthly temporal resolution offered here is based on 16-day composites of MODIS NDVI and EVI at 1 km grid resolution. Radiative transfer modeling and a number of filters were used to mitigate or eliminate cloud and aerosol effects. Particularly, for EVI effects of smoke and sub-gridscale thin clouds are taken into account. A short overview about validation activities can be found here.

The data set offered here contains 4 different quality flags; one gives general information about whether the quality is good or acceptable, in the latter case the recommendation is to look into the detailed quality flags, whether there is snow/ice present, or whether data are missing or have not been processed or have been filled with values from climatology. The second quality flag gives more detailed information about the quality (low value = low quality, high value = high quality). The two remaining flag give information about the aerosol load and/or the aerosol model used to correct the observed radiances and the second one details how many useful NDVI or EVI values of the 1 km grid resolution product contribute to CMG-grid data set given here.

 

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Contact

Antje Tittebrand

Institute of Oceanography, University of Hamburg, Hamburg

E-Mail: antje.tittebrand@we dont want spamzmaw.de

 

LP DAAC User Services

U.S. Geological Survey (USGS)

Center for Earth Resources Observation and Science (EROS)

E-Mail: LPDAAC@we dont want spameos.nasa.gov

 

Stefan Kern

ICDC, CliSAP, Universität Hamburg

E-Mail: stefan.kern@we dont want spamzmaw.de

 

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Data citation

Upon using this data please cite as follows:

These data are originally distributed by the Land Processes Distributed Active Archive Center (LP DAAC), located at the U.S. Geological Survey (USGS) Earth Resources Observation and Science (EROS) Center (lpdaac.usgs.gov), distributed in netCDF format by the Integrated Climate Data Center (ICDC, http://icdc.zmaw.de) University of Hamburg, Hamburg, Germany.

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