That means building the global scientific network to
monitor changes in the ocean's vital signs: pH, temperature and dissolved oxygen.
Not exact matches
The centre runs research programmes
in climate variability and
change, the
monitoring of sea levels,
ocean uptake of carbon dioxide, and Antarctic marine ecosystems.
Early
in April, Europe will launch the first satellite
in its Copernicus program: a fleet of a dozen environmental
monitoring spacecraft designed to study Earth's
oceans,
changes in land use, and atmosphere.
With so many instruments on the Yahtse, researchers have a unique opportunity to
monitor changes along the length of the glacier and discover how, for example, local
changes in ocean temperature and currents relate to movement further up the glacier.
The maps could also be useful resources for deciding where to place instruments to
monitor ocean oxygen levels
in the future to get the best picture of climate
change impacts.
The conferences have focused on international
ocean affairs with topics ranging from arms control, and
monitoring and surveillance
in the
oceans to management and conservation of marine resources; the feasibility of common shipping lines or on
ocean development tax; and more recently on emerging issues and challenges presented by climate
change, coastal cities and
ocean related hazards.
Rising CO2 emissions, and the increasing acidity of seawater over the next century, has the potential to devastate some marine ecosystems, a food resource on which we rely, and so careful
monitoring of
changes in ocean acidity is crucial.
Heavy metals and other pollutants could be
monitored in wastewater and
oceans could be
monitored for acidification due to climate
change.
Scientists from the Arctic
Monitoring and Assessment Programme (AMAP)
monitored widespread
changes in ocean chemistry
in the region.
Sea surface temperature (SST) measured from Earth Observation Satellites
in considerable spatial detail and at high frequency, is increasingly required for use
in the context of operational
monitoring and forecasting of the
ocean, for assimilation into coupled
ocean - atmosphere model systems and for applications
in short - term numerical weather prediction and longer term climate
change detection.
The overarching goal of this WCRP research effort, led by WCRP's Core Project «Climate and
Ocean Variability, Predictability and
Change» (CLIVAR) as a Research Focus, is to establish a quantitative understanding of the natural and anthropogenic mechanisms of regional to local sea level variability; to promote advances
in observing systems required for an integrated sea level
monitoring; and to foster the development of sea level predictions and projections that are of increasing benefit for coastal zone management.
This new sensory data would crucially advance knowledge
in monitoring global climate
change and tsunamis
in the deep
ocean.
To conduct the research, a team of scientists led by John Fasullo of the US National Center for Atmospheric Research
in Boulder, Colorado, combined data from three sources: NASA's GRACE satellites, which make detailed measurements of Earth's gravitational field, enabling scientists to
monitor changes in the mass of continents; the Argo global array of 3,000 free - drifting floats, which measure the temperature and salinity of the upper layers of the
oceans; and satellite - based altimeters that are continuously calibrated against a network of tide gauges.
Evidence for
changes in the climate system abounds, from the top of the atmosphere to the depths of the
oceans (Figure 2.1).1 Scientists and engineers from around the world have compiled this evidence using satellites, weather balloons, thermometers at surface stations, and many other types of observing systems that
monitor the Earth's weather and climate.
It allows us to better understand the current state of the
ocean, to
monitor trends
in temperature and salinity as climate
change continues, and to assess the skill of
ocean models.
In particular there could be significant heat storage changes deeper in the ocean that are inadequately monitored by the existing ocean networ
In particular there could be significant heat storage
changes deeper
in the ocean that are inadequately monitored by the existing ocean networ
in the
ocean that are inadequately
monitored by the existing
ocean network.
For further reading Arctic
Ocean Circulation Primer http://www.whoi.edu/page.do?pid=12317&tid=282&cid=23446 A New Way to
Monitor Changes in the Arctic http://www.whoi.edu/oceanus/viewArticle.do?id=33006 Is Global Warming
Changing the Arctic?
The endemic cloud cover at high latitudes prevents
monitoring of
ocean temperatures by IR radiometers, and microwave radiometers provide the only way to continually measure SST
in these vital Arctic regions, which are now experiencing rapid climate
change.
Monitoring trends
in biogeochemical indicators such as chlorophyll, dissolved oxygen, and nutrient concentrations is crucial for evaluating the
oceans» response to global climate
change and its effects on marine ecosystems.
The report, the most precise yet thanks to advances
in scientific
monitoring, confirms that climate
change impacts are outpacing previous projections for
ocean warming, the rate of glacial ice melt
in the arctic, and sea level rise.