Map developed by MACBIO for the bioregions workshop 2018. Chlorophyl-a concentration is an important proxy which is routinely measured and is considered a "core" parameter of global physical-biological oceanic models.
This map was developed by MACBIO as resource for the bioregions workshop 2017 and shows ocean surface currents based on data from NOAA Ocean Surface Current Analysis (http://www.oscar,noaa.gov/).
The map shows the diffuse attenuation coefficient per metre of depth (2002-present). This is an indicator of turbidity in the water column. The map was developed by MACBIO as resource for the bioregions workshop in Feb 2018.
A map showing the frontal index in Solomon Islands EEZ. The map was created by MACBIO as resource for the bioregions workshop in Feb 2018. Data is based on CSIRO Atlas of regional seas (CARS).
A front is a boundary between two distinct water masses that move in different directions.
This map was created by MACBIO as resource for the bioregions workshop in Feb 2018. The map represents the number of times a front has been detected in Sea Surface Temperature. Data is based on Moderate Resolution Imaging Spectroradiometer (MODIS).
Several maps showing a number of different chemical properties of the ocean, like nitrate concentration, oxygen concentration, ph, phosphate concentration, inorganic carbon concentration, Particulate organic carbon concentration, silicate concentration, surface temperature, radiation availability, mixed layer depth, phytoplankton concentration, available radiation and productivitiy.
These maps were developed by MACBIO as resource for the bioregions workshop in Feb 2018.
This thesis used a combination of sediment, coral, fish, climatic, and oceanographic data, and focused on the Pohnpei Lagoon, examining a range of natural and human issues in the marine environment both at the local level (focusing on that within the Pohnpei Lagoon) and regional level (focusing on the western Pacific region).
This report describes the high-resolution bathymetric mapping survey carried out in 2004. The survey achieved good coverage of the seafloor from approximately 10 m depth in the nearshore reef slope area, to an average offshore depth of some 2000 m, at an average slope angle of 2. The objective was to investigate the seabed and provide information about water depths around the islands using a multibeam echosounder (MBES).