Global EVI from Spring to Winter
Traditional satellite-based mapping of vegetation vigor and amount is based on the way vegetation interacts with red and infrared light. Occasionally, however, those two signals are not enough. MODIS measures light reflected from Earth at a variety of wavelengths, and the Arizona researchers incorporate the additional information into their Enhanced Vegetation Index (EVI). The EVI has increased sensitivity within very dense vegetation, and it has built-in corrections for several factors that can interfere with the satellite-based vegetation mapping, like smoke and background noise caused by light reflecting off soil.
The bi-weekly and monthly vegetation index maps have wide usability by biologists, natural resources managers, and climate modelers. They can track naturally occurring fluctuations in vegetation, such as seasonal changes, as well as those that result from land use change, such as deforestation. The EVI can also monitor changes in vegetation resulting from climate change, such as expansion of deserts or extension of growing seasons.
Global view of vegetation variation from Spring, 2000 through Winter, 2001.
Global EVI in Fall, 2000.
Global EVI in Spring, 2000.
Global EVI in Summer, 2000.
Global EVI in Winter, 2001.
Video slate image reads "EVI for Earth taken by Terra/MODIS Spring 2000 through Winter 2001".
Credits
Please give credit for this item to:
NASA/Goddard Space Flight Center
Scientific Visualization Studio
-
Animator
- Joycelyn Thomson (NASA/GSFC)
-
Scientists
- Alfredo Huete (The University of Arizona)
- Kamel Didan (The University of Arizona)
-
Writer
Release date
This page was originally published on Thursday, December 20, 2001.
This page was last updated on Wednesday, May 3, 2023 at 1:57 PM EDT.
Missions
This page is related to the following missions:Datasets used
-
[Terra: MODIS]
ID: 116
Note: While we identify the data sets used on this page, we do not store any further details, nor the data sets themselves on our site.