NOTICE -- The LBA-ECO Project website is no longer being supported.  This archive is a snapshot, as it existed in 2013, of the LBA-ECO website, maintained by NASA Goddard Space Flight Center, and now archived at the ORNL DAAC.  Links to external websites may be inactive. Final data products from the LBA project can be found at the ORNL DAAC.
banner
banner banner banner banner banner banner
banner banner banner banner banner banner banner
home aboutlibrarynews archivecontacts banner

spacer
banner
Investigations
Overview
Abstracts & Profiles
Publications
Research Sites
Meetings
Synthesis Groups
LBA-HYDROMET
LBA-Air-ECO
Logistics
Overview
Field Support
Travel
Visa
Shipping
Data
  Overview
Find LBA Data
Investigator Checklist
Process & Policy
Documentation & Archive
Training & Education
  Overview
Activities Summary
T&E Goals
Student Opportunities
  Folha Amazônica
 
spacer

Investigation:

LC-07 (Melack / Novo / Forsberg)

LBA Dataset ID:

LC07_LAKE_CHLORO

Originator(s):

1. NOVO, E.M.L.M.
2. BARBOSA, C.C.F.
3. FREITAS, R.M.
      4. SHIMABUKURO, Y.E.
5. MELACK, J.M.
6. FILHO, W.P.

Point(s) of Contact:

ORNL DAAC User Services Office Oak Ridge National Laboratory Oak Ridge, Tennessee 37 (ornldaac@ornl.gov)

Dataset Abstract:

This data set contains chlorophyll concentration maps of the Amazon River floodplain region from Parintins (Amazonas) to Almeirim (Para). These chlorophyll fraction maps were derived from the Moderate Resolution Imaging Spectroradiometer (MODIS) surface reflectance product (MOD09) for 19 months from April 2002 to December 2003.
The study was conducted in a floodplain reach upstream from Santarem, Para, in order to assess seasonal changes in phytoplanktonic chlorophyll-a distributions in the floodplain Lake Curuai. MODIS reflectance data were acquired at four river stages: rising (April), high (June), decreasing (September), and low (November). Chlorophyll maps were derived and used to compute the weighted average of chlorophyll concentration from MODIS images in the region. Field measurements of suspended inorganic matter and chlorophyll-a in Lake Curuai were made almost concurrently with satellite overpasses (Barbosa, 2005). The images and the estimated chlorophyll concentrations were compared to measured chlorophyll concentrations at control points for different hydrological states. This data set may be applied to better understand the seasonal dynamics of primary production of the Amazon floodplains. The maps of chlorophyll-a concentration may be used to model spatial and temporal variations of primary production in this region. The monthly chlorophyll-a maps are provided as GeoTIFF files. There are two formats: (1) color-mapped pixels and (2) pixels as chlorophyll-a concentrations. These latter images are not intended for browsing. These images have pixel values that are the chlorophyll-a concentration in mg/m3 and need to be download and opened in GIS software.

Beginning Date:

2002-04-01

Ending Date:

2003-12-31

Metadata Last Updated on:

2011-03-07

Data Status:

Archived

Access Constraints:

PUBLIC

Data Center URL:

http://daac.ornl.gov/

Distribution Contact(s):

ORNL DAAC User Services Office Oak Ridge National Laboratory Oak Ridge, Tennessee 37 (ornldaac@ornl.gov)

Access Instructions:

PUBLIC

Data Access:

IMPORTANT: The LBA-ECO Project website is no longer being supported. Links to external websites may be inactive. Final data products from the LBA project can be found at the ORNL DAAC. Please follow the fair use guidelines found in the dataset documentation when using or citing LBA data.
Datafile(s):

LBA-ECO LC-07 Amazon Floodplain Lake Chlorophyll from MODIS, Para, Brazil: 2002-2003:  http://daac.ornl.gov/cgi-bin/dsviewer.pl?ds_id=1000

Documentation/Other Supporting Documents:

LBA-ECO LC-07 Amazon Floodplain Lake Chlorophyll from MODIS, Para, Brazil: 2002-2003:  http://daac.ornl.gov/LBA/guides/LC07_Lake_Chlorophyll_MODIS.html

Citation Information - Other Details:

Novo, E.M.L.M., C.C.F. Barbosa, R.M. Freitas, Y.E. Shimabukuro, J.M. Melack, W.P. Filho. 2011. LBA-ECO LC-07 Amazon Floodplain Lake Chlorophyll from MODIS, Para, Brazil: 2002-2003. Data set. Available on-line [http://daac.ornl.gov] from Oak Ridge National Laboratory Distributed Active Archive Center, Oak Ridge, Tennessee, U.S.A. doi:10.3334/ORNLDAAC/1000

Keywords - Theme:

Parameter Topic Term Source Sensor
CHLOROPHYLL LAND SURFACE LAND USE/LAND COVER TERRA (MORNING EQUATORIAL CROSSING TIME SATELLITE) MODIS (MODERATE-RESOLUTION IMAGING SPECTRORADIOMETER)
LAKES LAND SURFACE LAND USE/LAND COVER TERRA (MORNING EQUATORIAL CROSSING TIME SATELLITE) MODIS (MODERATE-RESOLUTION IMAGING SPECTRORADIOMETER)
WETLANDS LAND SURFACE LAND USE/LAND COVER TERRA (MORNING EQUATORIAL CROSSING TIME SATELLITE) MODIS (MODERATE-RESOLUTION IMAGING SPECTRORADIOMETER)

Uncontrolled Theme Keyword(s):  AMAZON, AMAZON FLOODPLAIN LAKES, CHLOROPHYLL DISTRIBUTION, MODIS, REMOTE SENSING

Keywords - Place (with associated coordinates):

Region
(click to view profile)
Site
(click to view profile)
North South East West
  PARA WESTERN (SANTAREM) -1.00000 -3.00025 -52.99950 -57.00000

Related Publication(s):

Novo, E.M.L.M., C.C.D. Barbosa, R.M. de Freitas, Y.E. Shimabukuro, J.M. Melack, and W. Pereira. 2006. Seasonal changes in chlorophyll distributions in Amazon floodplain lakes derived from MODIS images. Limnology 7(3):153-161.

Data Characteristics (Entity and Attribute Overview):

Data Characteristics:

Images are provided for 19 months from April 2002-December 2003.



The monthly chlorophyll maps are provided as GeoTIFF files. There are two formats: (1) color-mapped pixels and (2) pixels as chlorophyll-a concentrations. These latter images have pixels in floating point (32 bit/pixel; binary values) and are not intended for browsing. Download these and open in GIS software such as ENVI, SPRING, or ArcGIS.



The GeoTIFF files are georeferenced by their upper left hand corner coordinate (57W, 1S). Pixels are equal-angle, in geographic LAT/LON, not map projected. Pixel size is 0.00225 degrees.



Also, the 19 pixels as chlorophyll-a concentration maps have been combined into a single 19 band GeoTIFF file.



Files:



RIO_MasCla_PHYChl_mmmyyyy.tif:



There are 19 color-scaled images where mmmyy is the month and year.



These color mapped images use the color legend as in Novo, 2006. Each of the color_scaled GeoTIFF images has 3 bands as rgb.The DN of the pixels indicate the color and the colors are quantized as in the legend. These color-mapped images have corresponding actual chl-a concentrations in mg/m3 GeoTIFF files described below.

PHYTO_Chl_mmm_yyyy.tif:



There are 19 GeoTIFF files with pixels in floating point file format where mmm_yyyy is the month and year. These 32 bit pixel values are the actual chlorophyll-a concentration in mg/m3. To display these images a 0 to 255 linear stretch is recommended.



PHYTO_Chl_X.tif: This file has the 19 separate pixels as chlorophyll-a concentration files combined into a single GeoTIFF file with 19 bands.

Data Application and Derivation:

This data set may be applied to better understand the seasonal dynamics of primary production of the Amazon floodplains. The maps of chlorophyll-a concentration may be used to model spatial and temporal variations in primary production in this region.



Three specific sources of data were used to derive this dataset. (1) MODIS / Terra - MOD09 product was used to map chlorophyll concentration. Medium resolution (250m x 250m) monthly images, MOD 09 Level 2 G Validated Version 3. (2) Chlorophyll field measurements, published in Barbosa, 2005, were used to calibrate the empirical mapping algorithm. (3) The MODIS data set was masked using a wetland mask (Hess et al. 2003) to limit the analysis to the floodplain. The Wetlands mask of the Central Amazon is a data set archived for this same LC-07 project.

Quality Assessment (Data Quality Attribute Accuracy Report):

Quality Assessment:

The regression equation expresses a nonlinear relationship between Chl and the phytoplankton fraction image. The standard error of estimate provided by the model is 19 mg m-3 and the adjusted R2 is 0.76; i.e., the model predicts, with an error of about 25%, chlorophyll concentration in the range between 10 and 120 mg m-3 in areas with suspended inorganic particle (ip) concentrations of 52 +/- 23 mg l-1. This range corresponds to digital numbers (DN) equivalent to chlorophyll fraction from 40 to 180.



To validate the empirical model suitability, it was applied to the image and the estimated chlorophyll concentration was compared to measured chlorophyll concentrations at control points for different hydrological states. There was a good agreement between the estimated and the measured chlorophyll concentration within the defined boundary conditions, which suggests that the model allows estimating the chlorophyll distribution provided that the class intervals are large enough to accommodate model variability.

Process Description:

Data Acquisition Materials and Methods:

Three specific sources of data were used to derive this dataset as described in Novo, 2006. (1) MODIS / Terra - MOD09 product was used to map chlorophyll concentration. Medium resolution (250m x 250m) monthly images, MOD 09 Level 2 G Validated Version 3. (2) Chlorophyll field measurements, published in Barbosa, 2005, were used to calibrate the empirical mapping algorithm. (3) The MODIS data set was masked using a wetland mask (Hess et al. 2003) to limit the analysis to the floodplain. The Wetlands mask of the Central Amazon is a data set archived for this same LC-07 project.



Site Description:

Curuaí Lake is composed of several depressions, which at high water coalesce into Lago Grande de Curuaí (1.5°S 55.43°W). It is located along the Amazon River, 900 km upstream from the river mouth at the Atlantic Ocean (Novo et al. 2006). The Amazon and the Tapajos rivers are the major sources of water to this floodplain. The lake receives different types of water, i.e., white water from the Amazon River during the overflow stage and black and clear water from the local catchments during the low stage (Barbosa 2005). The lakeâ�™s ecology is modulated by fluctuations in Amazon River water level.



Field Sampling:

From 2003 to 2004, field campaigns were undertaken to measure the concentrations of optically active components in Curuaí Lake. The campaigns spanned the seasonal changes in the Amazon Riverâ�™s hydrograph. The average time spent on each campaign was 10 days, with about seven stations sampled per day. The mean daily average concentrations of chlorophyll remained relatively constant during the period of each campaign (Barbosa, 2005).



To guide sampling, MOD 09 images were downloaded from the Land Processes Distributed Active Archive Center (LP DAAC), located at the U.S. Geological Survey EROS Data Center (http://LPDAAC.usgs.gov), before each field campaign to ensure that a representative range of chlorophyll concentrations was sampled. The position of samples was defined by examining historical Landsat-TM images representative of each water stage. For each date, at least 70 sites covering the entire lake were identified for determination of the concentration of chlorophyll (Chl), suspended inorganic particles (ip), and dissolved organic carbon (DOC).



MODIS (MOD09) Data Processing:

The MODIS data set was first masked to limit the analysis to the Amazonian floodplain study location. With the aid of Lake Curuai field samples of the 4 optically active components from open water, a series of prospective end-member pixel samples were selected to run a linear mixing model. Candidate end-member pixels were selected to decompose the MODIS data into proportions of reflected signals for each optically active component. It was determined that 3 end-members were appropriate; water (w), phytoplankton (phy), and inorganic particles (ip). From this, a linear mixing model was developed that incorporated the three optically active components to the reflectance values of each MODIS band. From one MODIS image, an empirical model was derived relating chlorophyll concentration measured in Lake Curuai to the phytoplankton (phy) contribution of the MODIS reflectance signal at a given pixel. Finally, this model was applied to the phytoplankton fraction images derived from the MOD09 data to compute the weighted average chlorophyll concentration in the region from Parintins (Amazonas) to Almeirin (Para) for 19 MODIS images from 2002 � 2003.

References:

Barbosa CCF (2005) Sensoriamento remoto da dinamica de circulao da agua do sistema planaA­cie de CuruaiaA­/Rio Amazonas. PhD thesis. National Institute for Space Research (INPE), Sao Jose dos Campos, Brazil.



Hess LL, Melack JM, Novo ELM, Barbosa CCF, Gastil M (2003) Dual season mapping of wetland inundation and vegetation for the central Amazon basin. Remote Sens Environ 87:404-428.doi:10.1016/j.rse.2003.04.001



Kirk JTO (1994) Light and photosynthesis in aquatic ecosystems, 2nd edn. Cambridge University Press, Cambridge. doi:10.1017/CBO9780511623370



Novo EMLD, Barbosa CCD, de Freitas RM, Shimabukuro YE, Melack JM, Pereira W. (2006) Seasonal changes in chlorophyll distributions in Amazon floodplain lakes derived from MODIS images. Limnology, 7, 153-161. doi:10.1007/s10201-006-0179-8



Nush EA (1980) Comparison of different methods for chlorophyll and phaeopigment determination. Arch Hydrobiol 4:14â�â�œ36

Skip navigation linksHOME | ABOUT | LIBRARY | NEWS ARCHIVE | CONTACTS | INVESTIGATIONS | LOGISTICS | DATA |TRAINING & EDUCATION

NASA logo
ORNL DAAC
Get Acrobat Reader