Climate and Chlorophyll a: Long-Term Trends in the Central North Pacific Ocean
- 2 October 1987
- journal article
- research article
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 238 (4823) , 70-72
- https://doi.org/10.1126/science.238.4823.70
Abstract
Since 1968 a significant increase in total chlorophyll a in the water column during the summer in the central North Pacific Ocean has been observed. A concomitant increase in winter winds and a decrease in sea surface temperature suggest that long-period fluctuations in atmospheric characteristics have changed the carrying capacity of the central Pacific epipelagic ecosystem.Keywords
This publication has 16 references indexed in Scilit:
- Estimates of Time and Space Scales at 300 Meters in the Midlatitude North Pacific from the TRANSPAC XBT ProgramJournal of Physical Oceanography, 1987
- The Ocean's Deserts Are BloomingScience, 1986
- Spatial patterns of chlorophyll, primary production, macrozooplankton biomass, and physical structure in the central North Pacific OceanJournal of Plankton Research, 1985
- Local Relationships between United States West Coast Precipitation and Monthly Mean Circulation ParametersMonthly Weather Review, 1984
- Environmental heterogeneity and plankton community structure in the central North PacificJournal of Marine Research, 1983
- Phytoplankton in an Oligotrophic Ocean: Observations and QuestionsEcological Monographs, 1982
- The lateral extent and characteristics of the North Pacific Central environment at 35°NDeep Sea Research Part A. Oceanographic Research Papers, 1979
- The deep chlorophyll maximum and mesoscale environmental heterogeneity in the western half of the North Pacific central gyreDeep Sea Research, 1978
- Oceanic habitat differences in The North PacificJournal of Experimental Marine Biology and Ecology, 1973
- A STUDY OF PLANKTON DYNAMICS AND NUTRIENT CYCLING IN THE CENTRAL GYRE OF THE NORTH PACIFIC OCEAN1Limnology and Oceanography, 1973