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Equatorial Pacific chemical and biological variability, 1997–2003
Citation
Strutton, PG and Evans, W and Chavez, FP, Equatorial Pacific chemical and biological variability, 1997-2003, Global Biogeochemical Cycles: An International Journal of Global Change, 22, (2) pp. 1-13. ISSN 0886-6236 (2008) [Refereed Article]
Copyright Statement
Copyright 2008 American Geophysical Union
Abstract
Using a database of roughly 300 basin-wide conductivity-temperature-depth (CTD)
stations per year from 1997 to 2003, we examined interannual and seasonal variability of
nutrients and chlorophyll across the equatorial Pacific. During this period, chlorophyll
concentrations exceeded the range of previous measurements for this region. Nitrate,
silicic acid, and phosphate also varied widely but not necessarily coherently with each
other or with chlorophyll. Across the La Nin˜a to El Nin˜o continuum there was
nonmonotonic variability in chlorophyll, particulate backscatter (a proxy for
phytoplankton carbon), and large size fraction (diatom) chlorophyll. In general, while El
Nin˜o was associated with decreased phytoplankton biomass, there was no corresponding
increase in phytoplankton or diatoms during La Nin˜a. However, there were increases
in macronutrients in response to La Nin˜a. We suggest that the lack of a biological
response to these nutrient increases is due to their decoupling from iron supply. Multiple
linear regression analysis of the physical factors responsible for vertical nutrient
fluxes emphasized the importance of winds in the central and western Pacific, and
thermocline depth in the east. We suggest that the role of the winds is not limited to
enhancement of upwelling, but perhaps more importantly to increased vertical mixing of
nutrients. Seasonal patterns were weak but consistent with previous work which has
suggested that enhanced productivity in the second half of the calendar year causes
reduced surface pCO2. Enhanced coverage of nutrient sensors on the tropical atmosphere
ocean (TAO) array would help to quantify seasonal signals associated with processes such
as tropical instability waves and lead to a better understanding of the links between
productivity, carbon export, and air-sea CO2 exchange.
Item Details
Item Type: | Refereed Article |
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Keywords: | equatorial pacific, biogeochemical cycling |
Research Division: | Earth Sciences |
Research Group: | Oceanography |
Research Field: | Biological oceanography |
Objective Division: | Expanding Knowledge |
Objective Group: | Expanding knowledge |
Objective Field: | Expanding knowledge in the earth sciences |
UTAS Author: | Strutton, PG (Professor Peter Strutton) |
ID Code: | 80201 |
Year Published: | 2008 |
Web of Science® Times Cited: | 31 |
Deposited By: | IMAS Research and Education Centre |
Deposited On: | 2012-10-24 |
Last Modified: | 2013-06-06 |
Downloads: | 0 |
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