As noted on the Data Fields Web page, the soil moisture data are scaled. Thus, you will need to multiply the data by 0.001 to obtain soil moisture in g cm-3.
Each frequency is looking at a different size footprint. Each frequency has its own feedhorn, and is thus susceptible to independent pointing errors. The most important benefit of resampling (or smoothing) is to create a suite of frequencies that are all looking at the same scene. So, when the higher-resolution channels are resampled to match the footprints of the lower-resolution channels, the data are smoothed.
In the not-resampled (unsmoothed) channels (denoted by ‘o‘ in Table 5):
- The unsmoothed 23.8 GHz channel does not spatially correlate with any other channels, and should generally not be used in conjunction with any other frequencies
- The 18.7, 36.5, and 89.0 GHz channels are not resampled to their own footprints, because it is intended that they be used in their native (not-resampled) form
- The 89A and 89B GHz channels are not aligned with the lower-resolution channels, by design
In the resampled channels (denoted by ‘•’ in Table 5):
- Pointing errors in the 6.9 and 10.7 GHz channels led to resampling of these channels to their own footprints in order to line their boresights up (or spatially correlate) with the higher-resolution channels
- The 23.8 GHz channel is resampled to spatially correlate with the 7.9, 10.7, and 18.7 GHz channels (it was determined that the footprint size of the 23.8 GHz channel was close enough to that of 18.7 that it did not warrant a suite of channels spatially correlated to the native 23.8 GHz footprint)
- For 18.7 and 36.5, each higher frequency is resampled to correlate with those native footprints
The unsmoothed and smoothed channels (see Table 5) are useful for constructing sets of “spatially correlated” channels, such as:
Resolution 1: 6.9, 10.7, 18.7, 23.8, 36.5, 89.0
Resolution 2: 10.7, 18.7, 23.8, 36.5, 89.0
Resolution 3: (18.7), 23.8, 36.5, 89.0
Resolution 4: (36.5), 89.0
Resolution 5: (89.0)
where, () = unsmoothed
Over homogeneous areas of ocean, the different size footprint observed by each frequency is not a big problem. But if there is heterogeneous meteorology, each channel may be looking at different amounts of cloud, rain, land, etc.
Start with the lowest frequency (largest footprint) that is important to any particular application.
For example, 10.7 GHz wind speed retrieval. Then ask, what would 18.7 GHz say if it were looking at the exact same patch of earth as this 10.7 GHz observation? And how bright would this exact same patch of earth (“scene”) be at 36.5 GHz?
The unsmoothed 18.7 and 36.5 GHz channels do not answer these questions directly, but there are more than enough observations to construct “virtual” observations which do “measure” the same scene. These are the smoothed channels.
You can find this information in this Online Support article.
The quality of a data set is very important to its user. Not knowing about data quality can lead to misleading interpretations and erroneous results. However, readily accessible data quality information enables the user to assess the limitations of a data set and to interpret the data accordingly.
Several of NSIDC’s data sets include quality information, which can range from flags, masks, or fields in the data or metadata to separate data quality summary files. Additional quality information is also often included in data set documentation and linked peer-reviewed literature. Thus, it can be a laborious process for data users to locate and interpret all of the quality information for a particular data set.
Fortunately, users of AMSR-E data sets can access all of this information in one convenient location. The new AMSR-E Data Quality Web pages provide information on the quality flags and files as well as data uncertainty reports provided by AMSR-E Principal Investigators. The data uncertainty reports are separated by parameter, such as sea ice and soil moisture, and provide the following:
- A synopsis on sources of uncertainty
- Best estimates of data uncertainty under optimal conditions for each measurement, including a confidence interval where possible
- A description of how to interpret quality flags to understand the conditions under which uncertainty may be greater
If you are an AMSR-E data user, check out this one-stop shop for data quality information.
Soil moisture is a key variable in understanding land surface hydrology and in modeling ecosystems, weather, and climate. Among NSIDC’s most popular data sets is the “AMSR-E/Aqua Daily L3 Surface Soil Moisture, Interpretive Parameters, & QC EASE-Grids” (AE_Land3) data set. This data set is distributed in HDF-EOS format and one of the biggest hurdles encountered by many users is simply learning how to display the data. Here are some tips on how to get started.
The HDF Group provides sample code for access and visualization of HDF data into IDL, MATLAB, and NCL. Access to the sample code for AMSR-E HDF data is provided on the HDF Group’s HDF-EOS Comprehensive Examples Web page.
If you are more familiar with GeoTIFF format, you may choose to utilize the HDF-EOS to GeoTIFF (HEG) Tool to convert AMSR-E Daily Soil Moisture HDF data into GeoTIFF format. This tool also allows you to subset the data with spatial or parameter constraints, as well as change the output projection. These HEG Tool services are also available as an option when ordering these data through the Reverb search and order interface. Instructions on how to use these data services in Reverb can be found in this Online Support article.
If you are interested in importing the data into ArcGIS, you can either use the GeoTIFF files generated by the HEG Tool or downloaded from Reverb, or you can perform a few steps to import the native HDF-EOS files into ArcMap. Using the ArcToolbox, you can easily extract a data field from an HDF file and save it in a different raster format that you are more familiar with. Instructions detailing how to do this can be found in this Online Support article.
New services that can be applied to AMSR-E and MODIS data have recently been added to the Reverb search and order tool. NASA Reverb|ECHO and NSIDC recently implemented these services in preparation for the decommissioning of the Data Pool search and order interface. Service options include reformatting the data from HDF-EOS to GeoTIFF, reprojection, and spatial or parameter subsetting. We created a tutorial to help data users access these data services.
The Data Pool search and order interface will be decommissioned on 28 August 2013. If you used the Data Pool search and order interface to reformat, reproject, or subset data, please use the new data services in Reverb. The Data Pool FTP site that provides direct access to data granules will remain available after the Data Pool search and order interface is decommissioned.
Hierarchical Data Format (HDF) supports a variety of data types and allows for the transfer and manipulation of scientific data across diverse operating systems and computer platforms. It was developed by the HDF Group at the University of Illinois and is the standard data format for all NASA Earth Observing System (EOS) data.
Despite the versatility of HDF, some data users have had difficulty in reading and displaying HDF data and often ask if we have sample code for reading HDF data in programs such as IDL and MATLAB.
Fortunately, the HDF Group provides sample code for access and visualization of HDF data into IDL, MATLAB, and NCL. Access to the sample code for NSIDC HDF data is provided on the HDF Group’s HDF-EOS Comprehensive Examples Web page.
Also note that this information can be found in our Online Support under the AMSR-E, MODIS, GLAS, and NISE forums.