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SOC shield2. Drivers and Trends for SOCD Research

2.5 Trends

Significant internal and external trends affect the Division's science and technology roadmap by influencing research, development, and integration approaches. Principal trends are highlighted below.

  • Integrated Ocean Observing System (IOOS)
    The U.S. Integrated Ocean Observing System will bridge the gap between operational remote sensing and in-situ stations in the United States. It is the United State's contribution to a Global Ocean Observing System (GOOS), which is a substantial component of the Global Earth Observing System of Systems (GEOSS). IOOS "is a coordinated national and international network of observations and data transmission, data management and communications, and data analyses and modeling that systematically and efficiently acquires and disseminates data and information on past, present and future states of the oceans and U.S. coastal waters to the head of tide." (First Annual Integrated Ocean Observing System (IOOS) Development Plan, A Report of the Nation Ocean Research Council Prepared by Ocean.US, The National Office for Integrated and Sustained Ocean Observations, Ocean.US Publication No. 9.) The Global Ocean Observing System (GOOS) will build on, enhance and supplement existing observing programs to develop a sustained and integrated observing systemthat provides the data and knowledge required to: manage and restore healthy coastal ecosystems and living resources; enable safer and more cost-effective marine operations; forecast and mitigate the effects of storms; detect and predict the effects of climate change; and protect public health. The Global Earth Observation System of Systems (GEOSS) is collaborative effort between 33 nations to share and blend in-situ and remotely-sensed Earth observations through existing and new compatible software and hardware. The U.S. and developed nations have a unique role in developing and maintaining the system, collecting data, enhancing data distribution, and providing models to help all of the world's nations.
    The national effort to establish an Integrated Ocean Observing System has assigned a significant leadership role to NOAA. The IOOS National Backbone includes satellite ocean remote sensing, where the nature of the roles for NOAA, NASA, and the Department of Defense in support of this satellite component is still being determined. NOAA clearly has a role in supporting IOOS with operational ocean remote sensing data. NOAA's role in providing data from developmental satellite programs is less clear. SOCD's NOAA CoastWatch/OceanWatch program for providing satellite ocean remote sensing data and products has been designated as a component of the IOOS National Backbone. The technology challenge is linking significantly increasing quantities of satellite ocean remote sensing data with IOOS and the IOOS Regional Associations. An IOOS science challenge is working with the IOOS Regional Associations to provide regional satellite ocean remote sensing data and products, with a significant focus on the coastal regime.
  • Collaborative Computing Environment
    Internal NOAA efforts are tending toward establishing a collaborative computing environment for satellite calibration/monitoring and product development, validation, and analysis. This new environment poses a notable technology challenge with respect to coordinating the numerous high-volume data streams and storage/archive requirements needed for implementing data quality assurance and scientific stewardship of climate data records.
  • Data Fusion
    Data fusion comprises, amongst other aspects, the blending of similar and complementary data sets to achieve "best value" data sets and the derivation of new parameters/information through combining different parameter data sets. Current illustrations of these types of efforts include: the blending of GOES and POES infrared SST data for a "best value" infrared SST data set; the blending of infrared and microwave SST data for the next-generation "best value" SST; and the combining of altimetry sea-surface height anomalies with scatterometry ocean surface winds to derive ocean surface currents.