Coastal Margin Observation and Prediction (CMOP) Program
Map of CMOP observation network in the lower estuary and coastal ocean.
CMOP Salmon Connection
CRITFC’s co-management ethos dictates that wherever the salmon go, we go with them. CMOP observations of water temperature and dissolved oxygen are directly relevant for salmon health. Observations of salinity are important for monitoring the risk of salinity intrusion into freshwater wetland habitat, particularly in the Cathlamet Bay, Oregon. CMOP modeling has been used to assess the potential effects on salmon due to changes in the Columbia River. CMOP modeling was used to assess potential water management regimes under the next Columbia River Treaty, and to assess the effects of proposed deepening of the Columbia River navigation channel in the early 2000s.
Virtual River Model
CMOP’s numerical model of the Columbia River estuary and coastal ocean (the Virtual Columbia River model) extends from Bonneville Dam to the open ocean. The primary focus is on the lower estuary and the river plume, which extends between 20 to 100 miles out into the ocean. The Virtual Columbia River is run as daily forecasts, 20-year historical simulations (‘hindcasts’), and scenario simulations such as sea level rise, channel deepening, or pre-development bathymetry. Model outputs are used to create indexes describing the estuary and plume, such as plume volume and salinity intrusion length, and climatology maps of salinity and temperature. Model outputs are also used to create estimates of potential juvenile salmon habitat and used in individual based modeling (IBM) of juvenile salmon migration. A new version of the model will include an improved representation the upper portion of the estuary and could be able to model water quality, sediment transport, and aquatic vegetation.
Virtual river modeling of bottom salinity (left) and surface salinity (right) of the Columbia River estuary.
SCHISM Modeling in the Pacific Ocean Basin
The National Ocean Service’s (NOS) operational ocean forecast models provide coastal flooding model guidance, forcing and boundary conditions for downstream models used by NOAA to forecast extreme weather, rip currents, storm surge, and flooding to protect people and property in the Pacific Ocean Basin. CMOP, in collaboration with NOAA, is developing and enhancing the surface current, tidal, and storm surge simulation capabilities in these models by extending the coverage both at the basin-scale and along the US coast and estuaries. By anchoring the modeling through high-resolution implementations of the unstructured-grid code SCHISM, enhancement of bathymetry, topography, shoreline, tidal gauge and external forcing data and products are being produced that will be integrated into future versions of the Extratropical Surge and Tide Operational Forecast System (ESTOFS).
Future of CMOP
CMOP has a long history operating in the estuary and is a known to the local community and to the regional oceanographic community. Through new partnerships, CMOP plans on expanding the understanding of the linkage between the ocean and estuary, both in terms of how it impacts the region’s salmon runs and quantifying the effects of climate change in this important and delicate ecosystem.
LinkVisit the CMOP website
Our co-management ethos dictates that wherever the salmon go, we go with them. [CMOP], alongside public and non-profit partners, brings tribal co-management and vision to the estuary and ocean environments.”
For More Information
Charles Seaton, CMOP Coordinator
A detailed description of the CMOP system is available in an open access reference paper.