Full catalog/NISAR_L2_GCOV_BETA_V1
NISAR_L2_GCOV_BETA_V1·v1·dataset

Processed radar surface texture, mapped (NISAR, beta)

NISAR Beta Geocoded Polarimetric Covariance Product (Version 1)
land NASA ASF Level 2 active HDF5PNGXMLPDF
In plain English

What it measures. This maps how radar energy scatters off the surface, including how the bounce-back changes with the radar's polarization, which reflects surface texture and structure. The numbers are corrected for terrain so slopes facing the radar do not falsely look brighter.

How it's made. Made from the NISAR mission's raw radar data, processed into a Level-2 product that is terrain-corrected and snapped onto a standard map grid.

How & where you'd use it. Helpful for studying land surfaces, vegetation and surface structure from radar; aimed at technical users. These are beta products meant for familiarization, not yet for scientific research.

What's measured

LAND SURFACE › GEOMORPHIC LANDFORMS/PROCESSESSOLID EARTH › TECTONICSAGRICULTURE › FOREST SCIENCECRYOSPHERE › GLACIERS/ICE SHEETSCRYOSPHERE › FROZEN GROUND

Coverage & cadence

  • Time span2025-10-01 → ongoing
  • Measured byNISAR (L-SAR, S-SAR)
  • Processing levelLevel 2
  • Spatial extent-180, -90, 180, 90
  • FormatsHDF5, PNG, XML, PDF, CSV, KML, YAML
  • StatusACTIVE

What you can do with it

  • Track deforestation, fire scars and land-cover change
  • Monitor crop and vegetation health (NDVI/EVI)
  • Map how built-up vs. green an area is over time
Official description

The NASA-ISRO Synthetic Aperture Radar (NISAR) Geocoded Polarimetric Covariance (GCOV) product is a Level 2 product derived from the Level 1 Range Doppler Single Look Complex (RSLC). The GCOV product provides terrain-corrected polarimetric covariance projected onto a predefined Universal Transverse Mercator (UTM) or polar stereographic projection system grid. RSLC radar samples, organized as a polarimetric scattering vector, are cross-correlated with the scattering vector’s conjugate transpose, originating the polarimetric covariance matrix expressed in the same grid as the RSLC range-Doppler grid. The magnitude of the resulting polarimetric covariance terms is strongly affected by the topography, with areas facing the sensor becoming brighter and areas away from the sensor turning darker in the images, biasing covariance measurements. To reduce the effect of the topography, an area-based radiometric terrain correction (RTC) is applied over the covariance terms, normalizing the backscatter coefficient from beta-naught to gamma-naught. The normalized covariance terms are then geocoded onto the output grid using an area-based adaptive multilooking. Since the polarimetric covariance matrix is Hermitian, only the upper triangular covariance terms are provided. The diagonal terms of the polarimetric covariance matrix are real-valued, representing the radar backscatter associated with each polarimetric channel. The off-diagonal terms of the polarimetric covariance matrix are complex-valued and may or may not be present depending on the GCOV processing mode. The products in this collection are considered Beta products and are intended to enable users to gain familiarity with the parameters and the data formats. Beta products are not intended for use in scientific research.

Get the data

nisar_l2_gcov_beta_v1_access.py
import earthaccess
earthaccess.login(strategy="netrc")          # free Earthdata Login

results = earthaccess.search_data(
    short_name="NISAR_L2_GCOV_BETA_V1",
    version="1",
    bounding_box=(-122.5, 37.2, -121.8, 37.9),  # your area (W,S,E,N)
    temporal=("2024-01-01", "2024-12-31"),       # your dates
)
files = earthaccess.open(results)   # stream straight from ASF
Browsing CMR needs no login. Downloading or streaming bytes needs a free Earthdata Login + the earthaccess package.