NASA Distributed Active Archive Center (DAAC) at NSIDC


Moderate Resolution Imaging Spectroradiometer

MODIS Terra vs. Aqua

NSIDC distributes MODIS data from both the Terra and Aqua satellites. The Temporal Coverage Tables on the MODIS Data Versions Web page lists the date ranges covered by each satellite. In addition, the differences detailed in the following sections can help you choose which satellite meets your needs and preferences.

Algorithmic Differences

The MODIS snow mapping algorithm utilizes a Normalized Difference Snow Index (NDSI) to differentiate between snow and other features in a scene. The NDSI is a band ratio that exploits the spectral differences between snow in MODIS Band 4 (short-wave infrared) and Band 6 (visible).

Because 70 percent of the Band 6 detectors on MODIS Aqua failed shortly after launch, all MODIS Aqua snow products through Version 5 use Band 7 (2.1 µm) instead of Band 6 to calculate the NDSI. In addition, the MODIS test for snow in vegetated areas, which compares a Normalized Difference Vegetation Index (NDVI) with the NDSI, was disabled in these versions because using Band 7 yielded too many false snow decisions.

However, Version 6 has incorporated a Quantitative Image Restoration (QIR) algorithm (Gladkova et al.) to restore Aqua MODIS band 6 data to scientific grade. When the MODIS Science Team tested the snow algorithm using QIR band 6 data, the output Aqua fractional snow cover maps were both accurate and equal in quality to the Terra maps. As such, Terra and Aqua now use the same snow detection algorithm based on band 6 data.

The sea ice mapping algorithm did not change from Terra to Aqua.

Orbital Differences

Differences in Terra's and Aqua's orbits result in different viewing and cloud-cover conditions for a given location. The following are some facts about both satellites:


The local equatorial crossing time is approximately 10:30 a.m. in a descending node with a sun-synchronous, near-polar, circular orbit. Visit the Terra Orbit Tracks Web site.


The local equatorial crossing time is approximately 1:30 p.m. in an ascending node with a sun-synchronous, near-polar, circular orbit. Visit the Aqua Orbit Tracks Web site.

Coverage Differences

The following examples show differences in coverage between Terra and Aqua over the European Alps on 15 February 2005. The top row shows orbital tracks, the middle row shows visible imagery, and the bottom row shows corresponding Level-2 (swath) snow extent data. Images derived from Aqua data normally appear upside-down due to Aqua's ascending orbit. In this case, the images were rotated 180 degrees for visual comparison with the Terra images.

Click the thumbnails for larger images.

Terra     Aqua
Aqua orbital tracks, 15 February 2005     Terra orbital tracks, 15 February 2005
10:30 local time
MOD021KM visible scene, 15 February 2005, 10:30
12:10 local time
MYD021KM visible scene, 15 February 2005, 12:10
MOD10_L2 image, 15 February 2005, 10:30     myd10_l2.20050215.1210.aqua.gif