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Caption for Image 1: Regional Changes in Ocean Chlorophyll

This graph shows the seasonal percent differences in ocean chlorophyll in the 12 major ocean basins between the early 1980s and the late 1990s, as recorded by satellites. The earlier records of ocean chlorophyll (1979 to 1986) were taken by the Coastal Zone Color Scanner (CZCS), while the more recent records (1997 to 2000) were measured by the Sea-Viewing Wide Field of View Sensor (SeaWiFS). Both datasets measured global ocean chlorophyll, the green pigment in plants that absorbs the Sun's rays for energy during photosynthesis, and both were also blended with surface observations of chlorophyll from ocean buoys and research vessels to reduce errors. An asterisk indicates that the difference is statistically significant. Credit: Watson W. Gregg (NASA) and Margarita E. Conkright (NOAA).

Caption for Images 2-4: Decadal Changes in Ocean Chlorophyll

These graphics show global maps of decadal changes in Ocean chlorophyll. To reduce errors, the data used to derive these maps was blended between satellite data and surface observations taken from buoys and research vessels. The top graphic shows blended Sea-Viewing Wide Field of View Sensor (SeaWiFS) satellite data of ocean chlorophyll concentrations during the summers (July to September) from 1997 to 2000. Concentrations are recorded in units of milligrams of chlorophyll per cubic meter (see side bar on right). The numbers on the left side of each image depict latitude, with zero being the equator and the negative numbers representative of southern latitudes. The numbers along the bottom of each image are longitude, and zero is the Greenwich meridian, the negative numbers indicate degrees west longitude. The middle graphic shows blended Coastal Zone Color Scanner (CZCS) data of ocean chlorophyll concentrations during the summers (July to September) from 1979 to 1986. The bottom graphic shows the differences in ocean chlorophyll between the SeaWIFS dataset and the CZCS record. Credit: Watson W. Gregg (NASA) and Margarita E. Conkright (NOAA)

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August 08, 2002 - (date of web publication)

SATELLITES SEE BIG CHANGES SINCE 1980s IN KEY ELEMENT OF OCEAN'S FOOD CHAIN

	Image 1

Since the early 1980s, ocean phytoplankton concentrations that drive the marine food chain have declined substantially in many areas of open water in Northern oceans, according to a comparison of two datasets taken from satellites. At the same time, phytoplankton levels in open water areas near the equator have increased significantly. Since phytoplankton are especially concentrated in the North, the study found an overall annual decrease in phytoplankton globally.

	Image 2

The authors of the study, Watson Gregg, of NASA's Goddard Space Flight Center, Greenbelt, Md., and Margarita Conkright, a scientist at the National Oceanic and Atmospheric Administration's (NOAA) National Oceanographic Data Center, Silver Spring, Md., also discovered what appears to be an association between more recent regional climate changes, such as higher sea surface temperatures and reductions in surface winds, and areas where phytoplankton levels have dropped.

	Image 3

Phytoplankton consist of many diverse species of microscopic free-floating marine plants that serve as food to other ocean-living forms of life. "The whole marine food chain depends on the health and productivity of the phytoplankton," Gregg said.

The researchers compared two sets of satellite data -- one from 1979 to 1986 and the other from 1997 to 2000 -- that measured global ocean chlorophyll, the green pigment in plants that absorbs the Sun's rays for energy during photosynthesis. The earlier dataset came from the Coastal Zone Color Scanner (CZCS) aboard NASA's Nimbus-7 satellite, while the latter dataset was from the Sea-Viewing Wide Field of View Sensor (SeaWiFS) on the OrbView-2 satellite.

	Image 4

The researchers re-analyzed the CZCS data with the same processing methods used for the SeaWiFS data, and then blended both satellite measurements with surface observations of chlorophyll from ocean buoys and research vessels over corresponding time periods. By doing so, the researchers reduced errors and made the two records compatible.

Results indicated that phytoplankton in the North Pacific Ocean dropped by over 30 percent during summer from the mid-80s to the present. Phytoplankton fell by 14 percent in the North Atlantic Ocean over the same time period.

Also, summer plankton concentrations rose by over 50 percent in both the Northern Indian and the Equatorial Atlantic Oceans since the mid-80s. Large areas of the Indian Ocean showed substantial increases during all four seasons.

"This is the first time that we are really talking about the ocean chlorophyll and showing that the ocean's biology is changing, possibly as a result of climate change," said Conkright. The researchers add that it remains unclear whether the changes are due to a longer-term climate change or a shorter-term ocean cycle.

Phytoplankton thrive when sunlight is optimal and nutrients from lower layers of the ocean get mixed up to the surface. Higher sea surface temperatures can reduce the availability of nutrients by creating a warmer surface layer of water. A warmer ocean surface layer reduces mixing with cooler, deeper nutrient-rich waters. Throughout the year, winds can stir up surface waters, and create upwelling of nutrients from below, which also add to blooms. A reduction in winds can also limit the availability of nutrients.

For example, in the North Pacific, summer sea surface temperatures were .4 degrees Celsius (.7 Fahrenheit) warmer from the early 1980s to 2000, and average spring wind stresses on the ocean decreased by about 8 percent, which may have caused the declines in summer plankton levels in that region.

Phytoplankton currently account for half the transfer of carbon dioxide from the atmosphere back into the biosphere by photosynthesis, a process in which plants absorb carbon dioxide (CO2) from the air for growth. Since carbon dioxide acts as a heat-trapping gas in the atmosphere, the role phytoplankton play in removing carbon dioxide from the atmosphere helps reduce the rate at which CO2 accumulates in the atmosphere, and may help mitigate global warming.

The paper appears in the current issue of Geophysical Research Letters.

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