We recognize that some users will find this file-size increase difficult to manage. Thus, we plan to add support for band-subsetting in the OBPG ordering system, but direct access distribution mechanisms will be delivering the full-band-suite Level-1A. This transition will occur with the reprocessing, so there will be a period of time when MODIS-Aqua is full-band and MODIS-Terra is subsetted.
The longitude and latitude datasets within the Level-2 products were previously provided in a sub-sampled form. They will now be full resolution. This simplifies usage by non-SeaDAS applications.
The fill-values have been standardized across datasets to simplify the identification of masked or
failed retrievals. In most cases, the derived product fields are now filled with -32767. Meta-data
attributes were added to each field to indicate the fill value both before and after any scaling
to integer. In the case where datasets are stored as scaled integers, the fill values are provided
for both the scaled and unscaled values.For the Rrs datasets, the solar irradiance is also included
in the meta-data (in units of mW/cm^2/um/sr)
to simplify conversion back to nLw (i.e., nLw = Rrs*solar_irradiance).
e.g.:
| int16 |
Rrs_670(Number of Scan Lines, Pixels per Scan Line) ; Rrs_670:long_name = "Remote sensing reflectance at 670 nm" ; Rrs_670:slope = 2.e-06f ; Rrs_670:intercept = 0.050000001f ; Rrs_670:units = "sr^-1" ; Rrs_670:solar_irradiance = 151.22081f ; Rrs_670:bad_value_scaled = -32767s ; Rrs_670:bad_value_unscaled = -0.015534f ; |
A processing version identifier was also added to the global attributes. For this reprocessing it the "pversion" attribute will be set to 2009.1.
Level-2 file names will now include the suite identifier (OC in this case). For example, a SeaWiFS Level-2 filename would be of the form Syyyydddhhmmss.L2_GAC_OC. This is to accomodate future product suites such as inherent optical properties (IOP).
The Level-3 binned file format used by the OBPG includes one or more geophysical parameters and
one set of statistics (i.e., number of observations, sum of weights, etc.) per bin. That means
that all parameters included in a given bin file must share the same exclusion criteria (masking).
It is therefore desireable to separate the geophysicical products into logical combinations
(or suites) with similar retrieval-failure rates.
For this reprocessing, the standard Level-2 OC products will be composited into a number of such logical groupings. The suite names and corresponding geophysical parameters are listed for each sensor below. The binned file names will now include the suite name (e.g., Syyyyddd.L3b_DAY_RRS.main).
| RRS suite | |
| aot_865 | aerosol optical thickness at 865-nm |
| angstrom | aerosol Angstrom exponent at 443-nm relative to 865-nm |
| Rrs_412 | remote sensing reflectance at 412-nm |
| Rrs_443 | remote sensing reflectance at 443-nm |
| Rrs_490 | remote sensing reflectance at 490-nm |
| Rrs_510 | remote sensing reflectance at 510-nm |
| Rrs_555 | remote sensing reflectance at 555-nm |
| Rrs_670 | remote sensing reflectance at 670-nm |
| CHL suite | |
| chlor_a | chlorophyll-a (OC4v5 algorithm) |
| KD490 suite | |
| Kd_490 | diffuse attenuation at 490-nm (KD2 algorithm) |
| PIC suite | |
| pic | particulate inorganic carbon (Gordon and Balch algorithm) |
| POC suite | |
| poc | particulate organic carbon (Stramski algorithm) |
| CDOM suite | |
| cdom_index | colored disolved organic matter index (Morel algorithm) |
| PAR suite | |
| par | daily mean photosynthetically available radiation (Frouin algorithm) |
| RRS suite | |
| aot_869 | aerosol optical thickness at 869-nm |
| angstrom | aerosol Angstrom exponent at 443-nm relative to 869-nm |
| Rrs_412 | remote sensing reflectance at 412-nm |
| Rrs_443 | remote sensing reflectance at 443-nm |
| Rrs_469 | remote sensing reflectance at 469-nm |
| Rrs_488 | remote sensing reflectance at 488-nm |
| Rrs_531 | remote sensing reflectance at 531-nm |
| Rrs_547 | remote sensing reflectance at 547-nm |
| Rrs_555 | remote sensing reflectance at 555-nm |
| Rrs_645 | remote sensing reflectance at 645-nm |
| Rrs_667 | remote sensing reflectance at 667-nm |
| Rrs_678 | remote sensing reflectance at 678-nm |
| CHL suite | |
| chlor_a | chlorophyll-a (OC3v5 algorithm) |
| KD490 suite | |
| Kd_490 | diffuse attenuation at 490-nm (KD2 algorithm) |
| PIC suite | |
| pic | particulate inorganic carbon (Gordon and Balch algorithm) |
| POC suite | |
| poc | particulate organic carbon (Stramski algorithm) |
| CDOM suite | |
| cdom_index | colored disolved organic matter index (Morel algorithm) |
| PAR suite | |
| par | daily mean photosynthetically available radiation (Frouin algorithm) |
| FLH suite | |
| ipar | instantaneous photosynthetically available radiation |
| nflh | fluorescence line height (normalized) |
The standard Level-3 mapped file format has been changed from a gridded 16-bit scaled integer array to a floating-point array. This was done to increase the science value of the mapped datasets, by delaying arbitrary scaling decisions until the point of actually generating a viewable image. In float format, the SMI product is effectively just a mapped version of the binned product. The SMI meta-data has also been changed to better support the float format. The global and SDS attributes of scaling, slope, and intercept are now set to "linear", 1.0, and 0.0, respectively, to ensure that software that blindly applies these values to "unscale" the mapped data (l3m_data SDS) back to float will have no effect. e.g.:
Parameter = "Chlorophyll a concentration" ;
Measure = "Mean" ;
Units = "mg m^-3" ;
Scaling = "linear" ;
Scaling Equation = "(Slope*l3m_data) + Intercept = Parameter value" ;
Slope = 1.f ;
Intercept = 0.f ;
Additional meta-data was added to provide a suggested scaling range that can be used by downstream applications to convert the float image into a byte-scaled image for display. This is the information that the OBPG uses to generate the Level-3 browse PNG images. e.g.:
Suggested Image Scaling Minimum = 0.01f ;
Suggested Image Scaling Maximum = 20.f ;
Suggested Image Scaling Type = "LOG" ;
Suggested Image Scaling Applied = "No" ;
The naming convention has also changed to capture the Level-3 product suite name and the approximate
resolution at the equator. Standard resolutions are still 9km and 4km for SeaWiFS and MODIS, respectively.
Projection is still equirectangular.As an example, a full set of SeaWiFS mapped files for one day (2005 day 264)
would look like this:
