Sea-viewing Wide Field-of-view Sensor (SeaWiFS)
Level 1A and Level 2 HDF
Dataset Guide Document
Version 2.0, June 2000
Coastal Regions of Chile and Argentina, Level 1A and Level 2 GAC Browse
Imagery
The Sea-viewing Wide Field-of-view Sensor (SeaWiFS) is an eight-channel
visible light radiometer dedicated to global ocean color measurements.
The mission parameters of SeaWiFS allow coverage of more than 90% of the ocean
surface every two days. SeaWiFS will map global ocean color at a resolution of
4.5 kilometers, and it also provides regional data at a resolution
of 1 kilometer. SeaWiFS is the follow-on mission to the Coastal Zone
Color Scanner (CZCS), and the predecessor to several ocean color satellite
sensors scheduled for deployment in the years 1998-2002.
Table of Contents
- Introduction
Sample Images
Abstract
- Investigators
Title of Investigation
Contacts
- Dataset Information
Introduction
Objectives/Purpose
Summary of Level 1 Parameters
Summary of Level 2 Geophysical Products
- Theory of Measurements
- Equipment
Instrument Description
Platform Description
Key Variables
Manufacturer of Instrument
Calibration
- Procedure
- Observations
- Data Granularity
- Data Description
Spatial Characteristics
Temporal Characteristics
Parameter/Variable Description/Definition
HDF Overview
- Data Analysis and Product Generation
General Discussion
Data Processing Sequence
- Errors
- Notes
- Applications of the Dataset
- Dataset Plans
- References
- Related Software
- Data Access
- Output Products and Availability
- Glossary of Terms
- List of Acronyms
-
- Dr. Charles McClain, Project Scientist
- Goddard Space Flight Center, Code 970.2
- Greenbelt, MD 20771
- (301)286-5377
- Email: mcclain@calval.gsfc.nasa.gov
- Dr. Wayne Esaias, MODIS Oceans Team Leader
- Goddard Space Flight Center, Code 971
- Greenbelt, MD 20771
- (301) 614-5709
- Email: wayne@puffin.gsfc.nasa.gov
- Dr. Stanford Hooker, Field Program Manager
- Goddard Space Flight Center, Code 971
- Greenbelt, MD 20771
- (301) 286-9503
- Email: stan@ardbeg.gsfc.nasa.gov
- Dr. Gene Feldman, Data System Manager
- Goddard Space Flight Center, Code 610.2
- Greenbelt, MD 20771
- (301) 286-9428
- Email:
gene@seawifs.gsfc.nasa.gov
Title of Investigation:
Sea-viewing Wide Field-of-view Sensor
Contacts (Data Production)
- Data:
- Dr. Gene Feldman
- Goddard Space Flight Center, Code 610.2
- Greenbelt, MD 20771
- (301)286-9428
- email: gene@seawifs.gsfc.nasa.gov
- Software:
- Frederick Patt
- SeaWiFS Project, Code 970.2
- Goddard Space Flight Center
- Greenbelt, MD 20771
- (301) 286-2866
- Email: Frederick.S.Patt.1@gsfc.nasa.gov
-
- Introduction:
This dataset consists of satellite measurements of global and
regional ocean color data obtained by the Sea-viewing Wide Field-of-view
Sensor (SeaWiFS), in orbit on the OrbView-2 (formerly "SeaStar") platform. The
concentration and predominant identity of substances and particles in the
euphotic (lighted) zone of the upper ocean influences the apparent color of the
ocean, which can range from deep blue to varying shades of green and ruddy
brown. Living phytoplankton (which contain chlorophyll and associated
photosynthetic pigments), inorganic sediments, detritus (particulate
organic matter), and dissolved organic matter all contribute to the color of
the ocean.
OrbView-2.
Objectives/Purpose:
A quantitative determination of global ocean primary productivity is
crucial to understanding the ocean's role in the global carbon cycle. The
SeaWiFS mission parameters were designed with this goal as a fundamental
consideration. In addition, SeaWiFS will refine remote-sensing measurements
of phytoplankton chlorophyll and associated pigments, organic matter,
and suspended particulate matter in the oceans. SeaWiFs will provide
the first continuous observations of global ocean color, anticipating
ocean color data from several future ocean remote sensing missions.
The Coastal Zone Color Scanner (CZCS) went far beyond its original
status as a proof-of-concept mission. During its eight years of operation
(November 1978-June 1986) the CZCS clearly demonstrated that measurements of
ocean color from space were possible, and also proved that this technology
could be used to characterize the distribution of biological productivity
in the surface ocean. CZCS mission constraints, however, prevented
quantitative determination of global ocean primary productivity.
NASA's ocean biogeochemistry research program, of which SeaWiFS
is a critical element, has established a set of science goals. Data from
SeaWiFS is expected to be used in the following ways:
- Goal I: Determine the spatial and temporal distributions of phytoplankton
blooms, along with the magnitude and variability of primary
production by marine phytoplankton on a global scale.
- Goal II: Quantify the ocean's role in the global carbon cycle and
other biogeochemical cycles.
- Goal III: Identify and quantify relationships between ocean physics
and large-scale patterns of biological productivity.
- Goal IV: Understand the fate of fluvial nutrients and their possible
effect on marine carbon budgets.
- Goal V: Identify the large-scale spatial and temporal distribution
of spring blooms in the global oceans.
- Goal VI: Acquire global data on marine optical properties, accompanied
by an improved understanding of processes associated with mixing
along the edges of eddies and boundary currents.
- Goal VII: Advance the scientific applications of ocean color data
and the technical capabilities required for data processing,
management, and analysis, in preparation for future missions.
One of the primary goals of the SeaWiFS Project is the following
stringent objective:
"To achieve radiometric accuracy to within 5% absolute and 1%
relative, water-leaving radiances to within 5% absolute, and
chlorophyll a concentration to within 35% over the range
0.05 - 50.0 mg m-3."
Summary of Level 1 Parameters:
Level 1 data consists of at-spacecraft raw radiance counts with
calibration and navigation information available separately in the data
file. The following table lists the center wavelength for each of the eight
SeaWiFS bands, along with the primary use of each wavelength. SeaWiFS
bands 1-6 are 20nm wide, and bands 7 and 8 are 40 nm wide.
Band Center Wavelength Primary Use
nm ("color")
1 412 (violet) Dissolved organic matter (incl. Gelbstoffe)
2 443 (blue) Chlorophyll absorption
3 490 (blue-green) Pigment absorption (Case 2), K(490)
4 510 (blue-green) Chlorophyll absorption
5 555 (green) Pigments, optical properties, sediments
6 670 (red) Atmospheric correction and sediments (CZCS heritage)
7 765 (near IR) Atmospheric correction, aerosol radiance
8 865 (near IR) Atmospheric correction, aerosol radiance
[ See Glossary for definitions of terms. ]
Summary of Level 2 Geophysical Products
Level 2 data consists of five normalized water-leaving radiances (radiance data
corrected for atmospheric light scattering and sun angles
differing from nadir), and seven geophysical parameters derived from the
radinace data. The following table lists the 11 SeaWiFS geophysical products.
Normalized water-leaving radiances at:
412 nm
443 nm
490 nm
510 nm
555 nm
670 nm
Chlorophyll a concentration
K(490)
Angstrom coefficient, 510-865 nm
Epsilon of aerosol correction at 765 and 865 nm
Aerosol optical thickness at 865 nm
[ See Glossary for definitions of terms. ]
Ocean color remote sensing is based on the principle that particulate
and dissolved substances suspended in water will interact with
incident light. Where concentrations of particulate matter and dissolved
substances are low, conditions typical for the open ocean,
water molecules scatter light similar to the way that the atmosphere scatters
light, producing a characteristic deep blue color. The scattering of light by
particulates and the absorption of light by dissolved substances will alter
this color. Chlorophyll, the photosynthetic pigment found in phytoplankton,
absorbs strongly in the red and blue regions of the visible light spectrum and
reflects in the green. As the concentration of phytoplankton increases,
the color of the water will therefore appear increasingly green. The
absorption of light by chlorophyll can be quantified to determine the
concentration of chlorophyll in water, allowing estimation of phytoplankton
abundance in a given area.
The relationship between light absorption and chlorophyll concentration may be
complicated by the presence of light-scattering inorganic particulate matter in
the water. Particulate matter concentrations generally increase in coastal
regions, such that the water color near the coast trends from green to brown or
reddish-brown. Even though chlorophyll may be present in higher concentrations
near the coast, the presence of particulate matter makes it more difficult to
extract the amount of light absorption due solley to chlorophyll. In addition,
certain classes of phytoplankton form hard mineral shells that scatter light
very effectively, such that the water color can appear shade of aquamarine or
milky white.
SeaWiFS measures light intensity in several bands. The measurements
allow quantification of light absorption and subsequent estimation of
chlorophyll and suspended matter concentrations. SeaWiFS improves on the
CZCS mission by having better bands for atmospheric correction (i.e.,
removing the effect of light scattering by the Earth's atmosphere), which
will particularly aid the estimation of chlorophyll and suspended matter
in coastal regions.
Instrument Description
The primary optics of SeaWiFS consist of an off-axis folded
telescope and a rotating half-angle mirror. Radiation backscattered by
the Earth's surface and atmosphere is collected by the telescope and
reflected onto the mirror, and the beam path is then directed through
beam splitters (dichroics, which transmit some wavelengths and reflect
the rest) to separate the radiation into four wavelength regions.
Spectral bandpass filters are used to narrow these regions to the 20 nm
requirements of the eight SeaWiFS spectral bands, and the radiation then falls
on silicon detector elements. The electronics module amplifies the detector
signal, performs analog-to-digital conversion and time delay and integration
for data transmission. Instrument calibration utilizes an on-board solar
radiation diffuser and lunar observation. The instrument may be tilted
forward or backward 20 degrees along the spacecraft orbital trajectory to
minimize the effects of sun glint.
SeaWiFS
Platform Description
The OrbView-2 satellite (formerly called "SeaStar") orbits in a
sun-synchronous, descending node orbit at an altitude of 705 km. The
orbital period is 98.9 minutes, with an inclination of 98.217 degrees.
Local time of descending node is 12:05 PM + 15 minutes.
The satellite was launched on August 1, 1997 into a 305 km orbit, and
32 orbit-raising burns performed over the next month raised the orbit
to its final altitude.
The satellite has a three-axis stabilized system consisting
of orthogonal magnetic torque rods for roll and yaw control and
two momentum wheels for pitch stabilization. The satellite is equipped
with sun sensors, horizon sensors, and magnetometers.
The propulsion system consists of two subsystems, a reaction control
system and a hydrazine propulsion system. The reaction control system uses
nitrogen and provides third stage stabilization during the launch. The
hydrazine propulsion system is used for raising the orbit from the nominal 278
km parking orbit to the 705 km sun-synchronous operational orbit. In addition,
it is used for orbit trim requirements over the life of the mission. The
spacecraft employs four Hamilton Standard one pound thrusters.
Redundant global positioning system (GPS) receivers are used for
orbit determination, an essential component of satellite and data navigation
(Earth location). The orbit state derived from GPS is included in the
spacecraft health telemetry.
Two telemetry streams are transmitted. The first is real-time LAC data
merged with spacecraft health and instrument telemetry at 665.4 kbps. This is
transmitted at L-band with a frequency of 1702.56 MHz. The other telemetry
stream consists of stored GAC and selected LAC, along with spacecraft health
and instrument telemetry, at 2.0 Mbps. This is transmitted at S-band with a
frequency of 2272.5 MHz. The command system uses S-band with an uplink of
19.2 kbaud at 2092.59 MHz.
Key Variables
Nominal operating parameters for SeaWiFS:
Scan Width 58.3 deg (LAC); 45.0 deg (GAC)
Scan Coverage 2,800 km (LAC); 1,500 km (GAC)
Pixels along Scan 1,285 (LAC); 248 (GAC)
Nadir Resolution 1.13 km (LAC); 4.5 km (GAC)
Scan Period 0.167 seconds
Tilt -20, 0, +20 deg
Digitization 10 bits
Manufacturer of Instrument
Hughes Electronics Santa Barbara Research Center
(Hughes SBRC)
Calibration
Pre-Launch Calibration
Due to the stringent radiometric objectives of the SeaWiFS Project,
SeaWiFS underwent an extensive prelaunch calibration program.
Calibration was performed at Hughes SBRC, and included an open
air observation of the Sun for solar calibration purposes. (The preflight
solar calibration is described in Chapter 3 of Volume 19 in the
SeaWiFS Technical Report Series, NASA Technical Memorandum 104566.)
The prelaunch characteristics of SeaWiFS were analyzed in detail
to provide a comprehensive understanding of the sensor's radiometric
response. SBRC employed a 100cm Spherical Integrating Source (SIS)
which with a spectral shape equivalent to a 2,850 K blackbody for
calibration purposes. Despite the approximate three-year hiatus between
instrument completion and spacecraft integration, the calibration
of the instrument was essentially unchanged over that time.
On-orbit calibration
SeaWiFS does not carry calibration lamps, but will rely on views
of a solar radiation diffuser and the moon for radiometric calibration.
The solar radiation diffuser is viewed once per orbit (near the southern
terminator) to monitor sensor calibration over several orbits. The
moon is viewed via a spacecraft maneuver to monitor calibration over months
or years. Lunar views take place when the lunar phase is few days prior to or
past full moon.
Data validation is accomplished by comparing data from the sensor
to ocean optical data obtained during a series of calibration cruises, both
prelaunch (commencing in 1992) and soon after the launch of the satellite.
The data validation process also utilizes data from the
Marine Optical Buoy
(MOBY) moored off of the island of Lanai, Hawaii. MOBY is a moored in- and
above-water optical radiometer that can transmit data to a receiving station on
Lanai, allowing frequent comparison to data from SeaWiFS.
Raw radiance data from the instrument is either transmitted
directly to ground High Resolution Picture Transmission (HRPT) stations or
recorded on the instrument for later transmission during downlink sessions to
GSFC. Direct broadcast data is 1 km resolution LAC data. Recorded data is
either 1 km resolution LAC data (primarily for calibration and validation)
and 4.5 km resolution GAC data. The GAC data is used for the production of
the global data set. Data is placed on disk and then processed to Level 1A,
Level 2, and Level 3 products by the SeaWiFS Project. The data are then
transmitted to the Goddard DAAC for archive and distribution. (HRPT data are
processed to Level 1A by the receiving station, then sent to the SeaWiFS
Project and subsequently to the DAAC.)
Missing Data
Although the SeaWiFS data set is essentially complete for the first 6 months of
operation, there are a few noteworthy gaps in coverage. During the initial
instrument check-out period from September 4 to September 18, 1997, the
instrument only collected data intermittently. From October 14-18, 1997, the
sensor was non-operational in "safe" mode due to transmission of incorrect
navigation data. During the reprocessing of the data in January 1997, a small
number of files were identified with large navigation errors that could not be
corrected. These files were deleted from the data archive.
Several short safe-hold periods have occurred during the mission. During November 1999
and November 2000, the instrument was turned off for several days, and the satellite orbital
configuration was adjusted to minimize the potential impacts of particles in the anticipated
peak Leonid meteor shower.
Masks and Flags
The SeaWiFS land mask is a 1 km resolution dataset that overlies all land areas
in the Level 2 product. Slight offsets may be found in the Level 1A LAC and
HRPT data up to approximately 2 pixels (~2 km). The bathymetry flag marks all
pixels from water depths less than 30 meters due to the possible influence of
bottom reflectance. The cloud/ice mask covers all pixels above an albedo
threshold. The cloud/ice mask may be misidentify shallow water areas with
particularly high albedo as clouds.
The following is a list (also found in the Operational Archive Product Specifications document)
of the algorithm name and corresponding flag condition for the l2_flags field in a SeaWiFS
version 3 data file:
ATMFAIL Atmospheric correction failure from invalid inputs
LAND Land (present in pixel)
BADANC Missing ancillary data
HIGLINT Severe Sun glint
HILT Total radiance above knee in any band
HISATZEN Satellite zenith angle above limit
COASTZ Shallow water
NEGLW Negative water-leaving radiance in any band
STRAYLIGHT Stray light contamination
CLDICE Clouds and/or ice
COCCOLITH Presence of coccolithophores
TURBIDW Turbid, case-2 water
HISOLZEN Solar zenith angle above limit
HITAU High aerosol concentration
LOWLW Low water-leaving radiance at 555 nm
CHLFAIL Chlorophyll concentration not calculable
NAVWARN Questionable navigation (e.g. tilt change)
ABSAER Absorbing aerosol index above threshold
TRICHO Presenc of Trichodesmium
MAXAERITER Maximum iterations of NIR algorithm
MODGLINT Moderate Sun glint
CHLWARN Chlorophyll out-of-range
ATMWARN Epsilon out-of-range
DARKPIXEL Dark pixel (Lt - Lt < 0) for any band
SPARE Spare flags
Due to the variety of SeaWiFS data products, the definition of
a data granule varies depending on the product. For Level 1A and Level
2 GAC data, the granule is a single swath of consecutive scans obtained as
the satellite orbit moves from the north polar region to the south polar
region. A single swath therefore contains approximately 40 minutes of
data. A single Level 1A data file is ~21.9 MB, and the corresponding
Level 2 file is ~19.1 MB.
For Level 1A HRPT data, the data granule contains the consecutive
scans broadcast to the station while the satellite was within the station's
receiving horizon. The 1 km resolution of HRPT LAC data makes the
file sizes much larger, in the range of 50-110 MB.
Spatial Characteristics
Coverage:
Spatial coverage is global, with full GAC coverage every two days.
(Cloud cover limits actual imaging of the entire ocean surface to
approximately every eight days, meaning that at least one view of any area on
the ocean surface can be obtained in an eight-day period.) Coverage along the
equator is slightly degraded due to instrument tilt to avoid sun glint effects.
Resolution:
L1A and Level 2 GAC has a spatial resolution at nadir of
4.5 km. Level 1A LAC data has a spatial resolution of
1.13 km, also at nadir.
Projection:
Level 1A HRPT, Level 1A GAC, and Level 2 GAC data have satellite swath
projection.
Temporal Characteristics
Coverage:
The archive of SeaWiFS data products began on September 18, 1997. Partial
orbit data was first obtained on September 4, 1997. Full-time operation of
SeaWiFS obtains approximately 14.5 swaths of Level 1A and Level 2 GAC data per
day, with each swath representing approximately 40 minutes of data (~20 MB).
Resolution:
The SeaWiFS rotating mirror rotates at a rate of 6 resolutions
per second, or 0.167 seconds per revolution. GAC scans represent
an Earth view of 21 milliseconds.
Parameter/Variable Description/Definition
SeaWiFS Level 1A data are raw radiance values for each of the
eight SeaWiFS bands, with calibration and navigation information
included in the HDF data file. Solar calibration and lunar
calibration data are available as separate HDF files. As for the
CZCS, a GAC pixel is generated by subsampling the LAC data
every fourth scan line and every fourth pixel, to generate an
effective GAC resolution of 4.5 km. Visible wavelength radiances
are measured for each of the 20nm wide SeaWiFs bands. The
bands are centered on the wavelengths given in the following table.
Band Center Wavelength Primary Use
nm ("color")
1 412 (violet) Dissolved organic matter (incl. Gelbstoffe)
2 443 (blue) Chlorophyll absorption
3 490 (blue-green) Pigment absorption (Case 2), K(490)
4 510 (blue-green) Chlorophyll absorption
5 555 (green) Pigments, optical properties, sediments
6 670 (red) Atmospheric correction and sediments (CZCS heritage)
7 765 (near IR) Atmospheric correction, aerosol radiance
8 865 (near IR) Atmospheric correction, aerosol radiance
Note: The SeaWiFS Level 1A browse product originally displayed the
raw radiance counts from band 8. The new browse product displays a pseudo
true-color image derived using data from bands 1, 5, and 6. The Level 1A GAC
browseproduct is subsampled by a factor of 2 to produce a 9 km resolution image.
SeaWiFS Level 2 GAC data consist of the following 11
geophysical products:
Normalized water-leaving radiances at:
- 412 nm
- 443 nm
- 490 nm
- 510 nm
- 555 nm
- 670 nm
And the following derived products:
- Chlorophyll a concentration
- K(490)
- Angstrom coefficient, 510-865 nm
- Epsilon of aerosol correction at 765 and 865 nm
- Aerosol optical thickness at 865 nm
Notes: The SeaWiFS Level 2 GAC browse product consists of the chlorophyll
a concentration values along with appropriate masks, and is 9 km
resolution (similar to the Level 1A browse product).
Normalized water-leaving radiances are corrected for the
effects of light scattering in the atmosphere and for sun angles
differing from nadir. Aerosol radiances are calculated as part
of the atmospheric correction process. The atmospheric
correction algorithm utilizes radiance data at 765 and 865 nm.
The chlorophyll a algorithm builds on the experience of CZCS and ocean optical
research during the intervening years, and will be subject to
refinement in the course of calibration and validation research. For version 3 data files, the
CZCS pigment geophysical product, which was simply the chlorophyll a value multiplied
by a constant, was deleted from the standard archive product. (See Aiken et al., 1995.) K(490)
also builds on the algorithms developed for CZCS data. The aerosol data products are derived
from the atmospheric
correction process. Version 3 data files add the Angstrom coefficient from 510-865 nm, which
is sensitive to aerosols.
Units of Measurement
Radiance units are milliwatts per square centimeter per micron per steradian
(mW cm-2 µm-2 sr-2).
Concentration units (for pigment and chlorophyll) are in milligrams
per cubic meter of seawater (mg m-3). K(490) is expressed
in units of reciprocal meters (m-1).
The epsilon of the aerosol correction, aerosol
optical thickness at 865 nm, and the Angstrom coefficient are dimensionless units.
Data Source
SeaWiFS orbits on the OrbView-2 satellite, which carried the
name "SeaStar" during most of the SeaWiFS development period.
OrbView-2 is a registered trademark of
Orbimage Inc.
HDF Overview
All SeaWiFS data is available in Hierarchical Data Format (HDF), a
data format developed by the
National Center for Supercomputing Applications (NCSA).
HDF is a "self-describing" data format, which means that all of the information
necesssary to examine the data in an HDF file is contained within the file.
HDF has several different "data models" which are used to store
data products. The data models that are used to store data are
Scientific Data Sets (SDS), Raster Image Sets, Vgroups, and
Vdatas. Global Attributes contain data that is applicable to the
entire data file. An entire HDF file may be visualized schematically
as a set of objects containing different data variables. Vgroups
act as directories to data arrays, and they can contain SDS objects.
HDF Structure of SeaWiFS Level 1A Data
For Level 1A data, the main object is a Scientific Data Set
(in this case, a three-dimensional array) containing the raw
radiances measured at the spacecraft for each pixel in a scan line,
for all 8 SeaWiFS bands. Thus, for a Level 1A LAC file, there are a
variable number of scan lines, each containing 1,285 pixels, with 8
radiance values associated with each pixel. L1A GAC data has 248
pixels per scan line due to the GAC subsampling scheme. Each L1A
GAC swath has approximately 3,600 scan lines, though this number is
not exact.
The Vgroups for SeaWiFS Level 1A data are:
Sensor Tilt
Converted Telemetry
Navigation
Scan-Line Attributes
Raw SeaStar Data
Calibration
The Vgroup "Raw SeaStar Data" contains the data object lla_data, the three-
dimensional array described above, as well as several variables that are
specific to each scan line.
(Refer to the PDF document
SeaWiFS OPERATIONAL ARCHIVE PRODUCT SPECIFICATIONS for information on the
variables of each of these Vgroups.)
SeaWiFS Level 1A Global Attributes:
Mission and Documentation
Product Name
Title
Data Center
Station Name
Station Latitude
Station Longitude
Mission
Mission Characteristics
Sensor
Sensor Characteristics
Data Type
Replacement Flag
Software Name
Software Version
Processing Time
Processing Control
Input Parameters
Data Time
Start Time
End Time
Scene Center Time
Node Crossing Time
Start Year
Start Day
Start Millisec
End Year
End Day
End Millisec
Start Node
End Node
Orbit Number
Data Quality
Pixels per Scan Line
Number of Scan Lines
LAC Pixel Start Number
LAc Pixel Subsampling
Scene Center Scan Line
Number of Scan Control Points
Number of Pixel Control Points
Mask Names
Flag Percentages
Scene Coordinates
Latitude Units
Longitude Units
Scene Center Latitude
Scene Center Longitude
Scene Center Solar Zenith
Upper Left Latitude
Upper Left Longitude
Upper Right Latitude
Upper Right Longitude
Lower Left Latitude
Lower Left Longitude
Lower Right Latitude
Lower Right Longitude
Northernmost Latitude
Southernmost Latitude
Westernmost Longitude
Easternmost Longitude
Start Center Latitude
Start Center Longitude
End Center Latitude
End Center Longitude
Orbit Node Longitude
HDF Structure for SeaWiFS Level 2 GAC Data
The structure of SeaWiFS Level 2 data is very similar to the
structure of Level 1A GAC data. There are only two new Global
Attributes, both in the Data Quality category: Mask Names and Flag
Percentages. The former indicates the different masks (such as
clouds or land) that were used in the processing. The latter indicates
how much of the data was flagged for not meeting specific quality
criteria during processing from Level 1 to Level 2. (Note that
Level 1A LAC data is not processed to Level 2.)
The primary new HDF object in the Level 2 GAC data is the
Vgroup "Geophysical Data", which contains 11 data arrays corresponding
to the pixel and scan line dimensions of the parent Level 1A GAC file.
Each array contains individual pixel values for each of the 11
SeaWiFS Level 2 geophysical products.
Related Datasets
The primary precursor dataset to the SeaWiFS dataset is the eight-year
archive collected by the CZCS. Other ocean color datasets are from the
Ocean Color and Temperature Scanner (OCTS) and the
Modular Optoelectronic
Scanner (MOS). The
Moderate Resolution Imaging Spectroradiometer (MODIS)
is slated to begin operations in 1998, and several additional ocean color
sensors are slated for launch in the period 1997-2002. Data from the
Advanced Very High Resolution Radiometer (AVHRR), primarily used to observe
sea surface temperature but also employed to observe turbid water masses,
can be correlated with ocean color data. Sea surface wind datasets (derived
either from remote sensing, meteorological instruments, or meteorological
observations) can also be used in concert with ocean color data.
General Discussion
The process of deriving accurate geophysical values from remote
sensing radiance data is conceptually simple yet operationally complex.
In principle, the instrument in space detects the intensity of light at
various wavelengths of the electromagnetic spectrum. In the case of
SeaWiFS, all of the wavelengths it detects are in the narrow segment of the
spectrum that is visible to the human eye. The sole function of the
instrument and its associated electronics is to quantify the light
intensity, translate it into digital form, append data that allows
the data to be navigated (i.e., determine the location on Earth from where
the light originated), and send it to an Earth-based receiving station.
The remainder of the data analysis takes place on Earth. Algorithms
developed on the basis of radiative transfer physics and
both oceanographic and meteorological observation are employed to accurately
extract the faint signal of backscattered light radiating from the ocean
surface from the pervasive influence of scattered light in the atmosphere, an
effect that is accentuated by the presence of atmospheric aerosol particles.
The CZCS employed the assumption that no light radiated
from the ocean surface at 670 nm, and thus all of the light detected was
due to Rayleigh scattering from air molecules and aerosol scattering. SeaWiFS
improves on this scheme by detecting light at 765 and 865 nm, as a small
amount of light may actually radiate from the ocean at 670 nm. Furthermore,
the atmospheric correction scheme used by SeaWiFS more accurately reproduces
variable atmospheric conditions (Gordon and Wang 1994).
Once the radiance signal has been corrected for atmospheric light scattering,
the signal is then corrected for the solar zenith angle to derive
normalized water-leaving radiances. Normalized water-leaving radiances are
subsequently used in algorithms to produce geophysical values. These
algorithms were developed through oceanographic research into the optical
characteristics of oceanic surface waters. As the most significant
influences on the optical nature of oceanic waters are the presence of
chlorophyll in phytoplankton and the presence of suspended particles, the
algorithms use the water-leaving radiances to calculate the values of the
related geophysical parameters. The geophysical parameters are calculated from
the radiance values on a pixel-by-pixel basis, allowing the values to be
mapped to Earth coordinates.
Several different methods have been employed to allow an accurate
continuous assessment of instrument calibration. These methods were
previously described in Section 5. The data analysis utilizes observations of
the onboard solar diffuser and of the nearly-full moon for onboard instrument
calibration. Data from the Marine Optical Buoy (MOBY) moored off of Lanai,
Hawaii, is used to monitor the accuracy of "system calibration", which
refers to the interaction of sensor data and scientific data processing
to derive geophysical values that approximate reality.
Data Processing Sequence
SeaWiFS Level 0 data is digitized at 10 bits for transmission
to ground stations. The primary data elements in Level 0 data are the
raw radiance counts for all eight bands, accompanied by spacecraft and
instrument telemetry. Processing to Level 1A appends calibration and
navigation data to the file, as well as instrument and selected spacecraft
telemetry. There are several different forms of Level 1A data: HRPT
LAC, recorded LAC (which includes several types of calibration data), and
GAC. A single GAC file consists of a swath data recorded from one
north-to-south orbital pass, and constitutes one HDF file. A single HRPT
file contains all of the scans received by the ground station while the
satellite was above the station's receiving horizon. Recorded LAC scans,
which are usually recorded for calibration and validation purposes as well
as for regions of special research interest, contain the number of scan
lines ordered by Mission Operations to cover the designated region.
Processing to Level 2 requires several additional steps. The
data is navigated so that land masks may be correctly placed. Ancillary
meteorological data and ozone data is used for atmospheric correction.
The computational steps described earlier are employed to produce normalized
water-leaving radiances and derived geophysical products. Each Level 2
data file is one HDF file, and corresponds exactly in temporal and spatial
extent to the parent Level 1A file. Note that only Level 1A GAC data is
processed to Level 2. Recorded LAC and HRPT LAC data is not processed to
Level 2, but the SeaWiFS Data Analysis System (SeaDAS), discussed
further in the "Related Software" section, will be capable of processing
Level 1A data to Level 2 geophysical products.
SeaWiFS data includes masks and flags for anomalous conditions.
The Level 1 to Level 2 data processing sequence tests for each of these
conditions, and either flags the data or places the appropriate mask.
Land, sun glint, and the presence of clouds and ice are masked.
The following is a list of the flag algorithms and masks with a brief
description of the condition that invokes them:
Flags:
- ATMFAIL
Atmospheric correction failure due to invalid inputs.
- HISOLZEN
Pixels with solar zenith angle greater than 75 degrees cause
uncertainty in atmospheric correction.
- HISATZEN
For pixels with pixel-to-spacecraft angles greater than 56 degrees,
causing distorted pixel sizes.
- STRAYLIGHT
Stray light (instrument effect) occurring in proximity to very bright pixels (high Lt).
- BADANC
Missing ancillary data: indicates if interpolated rather than real values for ozone or surface meteorological data were used.
- COASTZ
Water depth shallower than 30 meters where bottom reflectance effects
may occur.
- HITAU
High atmospheric turbidity indicator (aerosols), making atmospheric correction
less reliable.
- NEGLW
Negative water-leaving radiance: The normalized water-leaving radiance will be
set to zero for Level 3 binning. Can occur in cloud shadows, very high productivity Case 1 waters and turbid Case 2 waters.
- LOWLW
Normalized water-leaving radiance is below 0.15 mW cm-2
µm-2 sr-2 at 555 nm. Indicates an anomalous
condition as the water-leaving radiance is less than the clear water value.
- COCCOLITH
Indicates presence of coccolithophores (Brown and Yoder 1994).
- TRICHO
Indicates presence of Trichodesmium (Subramaniam et al., 2000)
- TURBIDW
Distinguishes Case 1 and Case 2 waters using an irradiance reflectance
algorithm (Morel 1988).
- CHLFAIL
Failure of the semi-analytic chlorophyll algorithm. Chlorophyll
concentration is set to zero for this case.
- NAVWARN
Questionable navigation; occurs most often in tilt segments.
- ABSAER
Absorbing aerosol index above a threshold of 0.5.
- MAXAERITER
The maximum number of iterations (10) for the NIR algorithm (Siegel et al., 2000) was exceeded.
- CHLWARN
Calculated chlorophyll values are out of range (0.001 - 64 mg m-3).
- DARKPIXEL
Dark pixel: Lt - Lt < 0 for any band.
- ATMWARN: Atmospheric Correction Failure
Atmospheric correction algorithm fails to return epsilon values
within a specified range.
Masks and Associated Flag Condition:
- HILT: High Lt
Radiances greater than the knee value in one or more bands, causing
reduced precision.
- LAND: Land
The flagged pixel is over land.
- CLDICE: Clouds and Ice
Pixels with an albedo at 865 nm greater than 1.1%.
- HIGLINT, MODGLINT: Sun Glint
Pixels with a glint radiance greater than 0.005F0(865) will be masked.
F0 is the extraterrestrial solar constant adjusted for Earth-Sun distance.
MODGLINT indicates that a sun glint correction was applied, and is a flag;
HIGLINT is a mask invoked by the condition defined above.
The conditions described above were designated for the purpose
of identifying and marking conditions that can make the data unreliable for
research purposes. After approximately four months of operation, the SeaWiFS Project evaluated the
data that had been obtained by the instrument and concluded that that sensor
had met the established criteria for mission success. As the SeaWiFS mission
continues and the algorithms are refined, the reliability and integrity of the
full dataset can be better assessed.
Several research projects managed by or in association with the
Calibration/Validation element of the SeaWiFS Project are intended to analyze
and refine SeaWiFS calibration and the algorithms used to produce
Level 2 geophysical products. During January and February 1998, the entire
dataset was reprocessed for the first time with improved algorithms and
instrument calibration data. These algorithms provided the first
science-quality SeaWiFS ocean color data, as the initial data produced with
the at-launch algorithm set were considered preliminary results. The SeaWiFS
Project plans to periodically reprocess the accumulated dataset using
algorithms developed by ongoing research efforts.
The dataset has been reprocessed two subsequent times: from October 1998 to April 1999, and in May-June 2000.
As stated earlier, the goals of the SeaWiFS Project are stringent
with regard to both radiometric accuracy and the accuracy of the primary
geophysical products. The stated goal for chlorophyll concentration is an
accuracy of 35% within the range 0.05 - 50.0 mg m-3.
The main application of SeaWiFS data is research into the dynamics
of phytoplankton populations in the surface waters of the ocean on a global
scale. This research is important to investigations of carbon cycling in the
ocean and the flux of carbon dioxide from the ocean to the atmosphere, which
in turn is an important factor in the global climate system.
SeaWiFS data is also very useful into research on phytoplankton
dynamics on the basin scale, mesocale, and even the fairly small
scale of river outflow and phytoplankton distribution in large lakes.
These types of investigations are very useful to marine ecosystem research,
fisheries, and localized perturbations in the marine environment. Furthermore,
SeaWiFS data on ocean clarity and turbidity can be used in investigations
of sediment transport processes and various forms of anthropogenic input
to the ocean.
On a fundamental level, SeaWiFS data allows a more detailed
investigation of the optical physics of seawater on a global scale.
It is anticipated that the data from SeaWiFS will be augmented
by data from the
Moderate Resolution Imaging Spectroradiometer (MODIS),
launched in December 1999 on the Terra platform. Several other countries
have ocean color sensors in development that are slated for launch in the
period 1998-2000. The
Sensor Intercomparison and Merger for
Biological and Interdisciplinary Oceanic Studies (SIMBIOS) project was formed
for the purpose of intercalibration of ocean color data obtained by different
ocean color instruments.
- Aiken, J., G.F. Moore, C.C. Trees, S.B. Hooker, and D.K. Clark, 1995:
The SeaWiFS CZCS-Type Pigment Algorithm.
SeaWiFS Technical Report Series, Volume 29, NASA Technical Memorandum
104566, S.B. Hooker and E.R. Firestone Eds., NASA Goddard
Space Flight Center, Greenbelt, Maryland, 34 pages.
- Biggar, S.F., P.N. Slater, K.J. Thome, A.W. Holmes, and R.A. Barnes,
1994: "Chapter 3: Preflight Solar-Based Calibration of SeaWiFS", IN:
McClain, C.R., R.S. Fraser, J.T. McLean, M. Darzi, J.K. Firestone, F.S. Patt,
B.D. Schieber, R.H. Woodward, E-n. Yeh, S. Mattoo, S.F. Biggar, P.N. Slater,
K.J. Thome, A.W. Holmes, R.A. Barnes, and K.J. Voss, 1994: Case Studies for
SeaWiFS Calibration and Validation, Part 2,
SeaWiFS Technical Report Series, Volume 19, NASA Technical Memorandum
104566, S.B. Hooker, E.R. Firestone, and J.G. Acker, Eds., NASA Goddard
Space Flight Center, Greenbelt, Maryland, 25-32.
- Brown, C.W., and J.A. Yoder, 1994: Coccolithophorid blooms in the global
ocean. J. Geophys. Res., 99, 7467-7482.
- Gordon, H.R., and M. Wang, 1994: Retrieval of water-leaving radiance and
aerosol optical thickness over the oceans with SeaWiFS: a preliminary
algorithm. Appl. Opt., 33(3), 443-452.
- Morel, A., 1988: Optical modeling of the upper ocean in relation to
its biogenous matter content (Case I waters). J. Geophys. Res.,
93, 10,749-10,768.
- Siegel, D.A., M. Wang, S. Maritorena, and W.D. Robinson, 2000: Atmospheric
correction of satellite color imagery: the black pixel assumption. Appl.
Opt., (submitted).
- Subramaniam, A., R.R. Hood, C.W. Brown, E.J. Carpenter, and
D.G. Capone, 2000: A classification algorithm for mapping
Trichodesmium blooms using SeaWiFS. Deep Sea Research, (submitted).
SeaDAS was specifically developed for the processing and analysis of
SeaWiFS HDF data. The following describes the what SeaDAS can do, as well
as providing a path to obtain the software.
The SeaDAS Web site, http://seadas.gsfc.nasa.gov,
is updated with current operating information for SeaDAS 4.0. System configuration and
hardware requirements, and information on how to obtain SeaDAS 4.0, are given
below and are also found on the SeaDAS Web site.
The SeaDAS software system was written for the specific purpose of analyzing and
processing SeaWiFS HDF data. SeaDAS is a comprehensive image analysis package
for all SeaWiFS data products and ancillary data (wind, surface pressure, humidity and
ozone) from NMC (National Meteorological Center and TOVS (TIROS Operational Vertical
Sounder). All SeaDAS source code is free and available for download via FTP.
The Interactive Data Language (IDL) from Research System Inc. (RSI)
is used to build all the GUI and display related programs in SeaDAS. SeaDAS 4.0 is released
with a blanket purchase of IDL-Runtime, so users do not have to acquire IDL or IDL-Runtime
at their expense. SeaDAS includes
the Hierarchical Data Format (HDF) libraries from National Center for Supercomputing
Applications (NCSA) which are also required to build certain SeaDAS programs. IDL, C,
FORTRAN77, and IMAKE from the vendors are required only if modifications to the source
code and user-defined versions of the executables are desired.
Suggested Hardware Requirements:
- Platform: SGI 02, SUN UltraSparc workstations, or PC
- Memory:192 MB (regular users), 384 GB (HRPT users)
- Disk: 9 GB (actual SeaDAS installation requires ~330 MB without demo files and
~950 MB with demo files. Additional disk space is required for storing original data and
processed data files.
- Tape Drive: 4MM(DAT) or 8mm Exabyte (for DAAC data)
- Display: 19" Console or X-terminal with 20 MB memory, 1280x1024 resolution, 8-bit, 256 colors
Software Requirements:
- Operating Systems: SGI: IRIX 6.3, or IRIX
6.5 SUN: Solaris 2.6 or Solaris 2.7
- Required Software: IDL-Runtime, IDL 5.1 or 5.2
- Languages: C (SGI V3.19, SUN V 3.0.1), FORTRAN(SGI V 4.0.2, SUN V
3.0.1), IDL 5.2 or 5.3 (IDL 5.1 may work but has not been re-tested)
- Software Libraries: HDF 4.1r1 (included in SeaDAS)
SeaDAS PC Linux Version
SeaDAS 4.0 for Linux/PC has been developed and tested under the following environment:
"Generic" PC with Pentium II 350 MHz CPU
Redhat Linux 6.0
IDL 5.1.2L for PC, IDL-Runtime
Compile-from-scratch support
- SGI: IRIX 6.3 and 6.5
- Sun: Solaris 2.6 and 2.7
- PC: RedHat Linux 6.0
Obtaining SeaDAS 4.0
SeaDAS is available for download via anonymous FTP from seadas.gsfc.nasa.gov.
The /seadas directory contains the following compressed tar files:
- seadas_data1.tar.Z, seadas_data2.tar.Z, seadas_data3.tar.Z: SeaDAS required data files for L1, L2, and L3 processing
- seadas_demo.tar.Z: sample files for testing, and demonstrations
- seadas_irix6.3.tar.gz: SeaDAS for SGI IRIX 6.3 operating system
- seadas_irix6.5.tar.gz: SeaDAS for SGI IRIX 6.5 operating system
- seadas_solaris2.6.tar.gz: SeaDAS for SGI IRIX 6.3 operating system
- seadas_irix2.7.tar.gz: SeaDAS for SGI IRIX 6.3 operating system
- seadas_rhlinux6.0.tar.gz: SeaDAS for PC, RedHat Linux 6.0 operating system
Connect to the SeaDAS ftp
site to download program files.
Note, some users, especially outside the U.S. have had trouble
with the size of large SeaDAS files. Smaller "split" sections of the files
have been created using the UNIX "split -20000" command. The split files can be found in the /seadas/split directory.
To put the split files back together (concatenate the files), use the following commands:
cat seadas_src.tar.Z?? > seadas_src.tar.Z (for source
tar file), OR
cat seadas_data.tar.Z?? > seadas_data.tar.Z (for data
tar file)
To put the pieces back together, and uncompress them, and unTAR the
TAR file in one step:
cat seadas_src.tar.Z?? | zcat - | tar xvf - (for source files)
OR
cat seadas_data.tar.Z?? | zcat - | tar xvf - (for data files)
SeaDAS can also be created on 4mm (DAT) or 8mm tape for those users who
do not have Internet access or who have substantial difficulty with FTP of
these large files. Please send your request to seadas@seadas.gsfc.nasa.gov.
Other HDF Software
SeaWiFS data has been successfully opened and examined using the
Fortner Research prototype HDF Browser. The
Research Systems Inc. software products Transform
and Noesys (descriptions can also be found at the SciSpy Web site) have been used on
SeaWiFS data files, and Noesys has been used to transfer SeaWiFS data to the EASI/PACE
Geographical Information System (GIS) software package.
Two other software packages, HDF Explorer and Windows Image Manager, have
also been used with SeaWiFS data files. Links to the sites where more
information can be obtained are below. Windows Image Manager offers the capability of
converting SeaWiFS data to many other image formats.
HDF Explorer
Windows Image Manager
The SeaWiFS project is a "data buy" mission, for which NASA contracted with
Orbital Sciences Corporation to build and launch the satellite. In return,
Orbital Sciences Corporation was granted the opportunity to sell data from
SeaWiFS for commercial applications. From September 18, 1997 to March 11,
1998, data from SeaWiFS was unrestricted. After March 11, 1998, the data is
restricted to
SeaWiFS Authorized Research Users solely for scientific research
purposes. The data is subject to a two-week distribution embargo for normal
research applications. Rea-time data access is granted to researchers and
selected HRPT stations for specific research needs. After five years, all
SeaWiFS data will be unrestricted.
In order to restrict data access to SeaWiFS Authorized Research Users,
usernames and passwords are issued from the Goddard DAAC to each individual
research user after they have provided the
necessary documentation to the SeaWiFS Project.
Contacts for Archive/Data Access Information
Goddard DAAC Ocean Color Data and Resources Website
/OCDST/OB_main.html
Goddard DAAC Ocean Color Data Support Team
ocean@daac.gsfc.nasa.gov
James Acker, Team Lead
Code 610.2
NASA Goddard Space Flight Center
Greenbelt, MD 20771
USA
ocean@daac.gsfc.nasa.gov
301-614-5435
FAX: 301-614-5268
Goddard DAAC Helpdesk
Frances Bergmann
Code 610.2
NASA Goddard Space Flight Center
Greenbelt, MD 20771
USA
daacuso@daac.gsfc.nasa.gov
301-614-5224
FAX: 301-614-5268
Archive Identification:
NASA Goddard Space Flight Center DAAC
-
-
Tape Media:
8mm EXABYTE tape (8200 and 8500 bpi)
4mm DAT tape (90m)
Other Products:
All SeaWiFS Products at the Goddard DAAC can be obtained by electronic
transfer using the File Transfer Protocol (FTP.)
aerosol:
a suspension of fine solid or liquid particles in gas
albedo:
reflective power, i.e., the fraction of incident radiation (as light)
that is reflected by a surface or body
algorithm:
a step-by-step procedure for solving a problem or
accomplishing some end especially by a computer
ancillary:
supplementary (ancillary data with regard to SeaWiFS refers to
data from other sources that is used in data processing)
backscatter:
the scattering of radiation or particles in a direction opposite to that of
the incident radiation due to reflection from particles of the medium
traversed, or the actual radiation due to this process
bathymetry:
water depth measurements in a given body of water
bloom:
a rapid increase in the population and concentration of phytoplankton
boundary current:
large strong surface ocean currents that occur on the margins of ocean
basins, usually flowing parallel to a continental coast
chlorophyll:
photosynthetic pigment found in plants. Chlorophyll a is a green
pigment.
coccolithophore:
phytoplankton which creates external microscopic calcium carbonate hard
plates (coccoliths)
descending node:
the point at which an orbiting body rises through the plane of the ecliptic
traveling southward
downlink:
a communications channel for receiving transmissions from a spacecraft;
eddy:
a feature of ocean circulation where the direction of circulation is
circular or elliptical
electromagnetic spectrum:
the entire range of wavelengths or frequencies of electromagnetic
radiation extending from gamma rays to the longest radio waves and
including visible light
euphotic:
of, relating to, or constituting the upper layers of a body of water into
which sufficient light penetrates to permit growth of green plants
fluvial:
related to streams or rivers
gelbstoffe:
Dissolved and suspended inorganic matter, commonly found in river
discharge, which gives it a yellowish color. (from German:
"yellow substance").
inclination (orbital)":
angle between the orbital plane and the Earth's equatorial plane,
measured in degrees
interpolation:
to estimate values of (a function) between two known values
irradiance:
the density of radiation incident on a given surface, irrespective
of direction
mask:
a single data value that indicates the presence of a particular
condition
nadir:
the point on the Earth directly below an orbiting satellite.
optical thickness:
the normalized extinction coefficient due to absorption and scattering
by intervening substances or particles in a direct beam of light
period:
the time interval required for the completion of one orbit by a satellite
photosynthesis:
the process by which chlorophyll-containing cells in plants convert incident
light to chemical energy and synthesize organic compounds from inorganic
compounds, especially carbohydrates, from carbon dioxide and water, with the
simultaneous release of oxygen.
phytoplankton:
free-floating photosynthetic organisms existing in aquatic environments
primary productivity
the rate at which organic carbon is produced photosynthetically.
radiance:
electromagnetic energy per unit time, area, solid area and spectral
band, i.e., electromagnetic energy radiating in a given direction
radiometer:
a device that detects and measures electromagnetic radiation in discrete
spectral bands of the electromagnetic spectrum.
resolution
In a spatial sense, the size of the smallest feature recognizable using the
detector.
spectral band:
a narrow range of the electromagnetic spectrum.
sun glint:
sunlight that is directly reflected from the water surface back
to the observer or detector
terminator:
the dividing line between the illuminated and the unilluminated part of the
moon's or a planet's disk
turbidity:
substances or particles that obscure light transmission
visible light:
Electromagnetic radiation with wavelength in the 390 to 770 nm range.
zenith:
the "sky" point located directly above an Earth-based sensor.
AVHRR Advanced Very High Resolution Radiometer
CZCS Coastal Zone Color Scanner
DAAC Distributed Active Archive Center
FTP File Transfer Protocol
GAC Global Area Coverage
HDF Hierachical Data Format
HRPT High Resolution Picture Transmission
LAC Local Area Coverage
MOBY Marine Optical Buoy
MODIS Moderate Resolution Imaging Spectroradiometer
MOS Modular Optoelectronic Scanner
NASA National Aeronautics and Space Administration
NCSA National Center for Supercomputing Applications
OCTS Ocean Color and Temperature Scanner
SBRC Santa Barbara Research Center
SDS Scientific Data Sets
SIMBIOS Sensor Intercomparison and Merger for Biological and
Interdisciplinary Oceanic Studies
SIS Spherical Integrating Source
SeaDAS SeaWiFS Data Analysis System
SeaWiFS Sea-viewing Wide Field-of-view Sensor
Change History
- Version 2.0
- Version baselined on addition to the GES Controlled Documents List, February 18, 2000.
- Version 2.0 created June 13, 2000.
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