Temporal variations in lower trophic level biological environments in the northwestern North Pacific Subtropical Gyre from 1950 to 1997

Citation
A. Limsakul et al., Temporal variations in lower trophic level biological environments in the northwestern North Pacific Subtropical Gyre from 1950 to 1997, PROG OCEAN, 49(1-4), 2001, pp. 129-149
Citations number
53
Categorie Soggetti
Earth Sciences
Journal title
PROGRESS IN OCEANOGRAPHY
ISSN journal
00796611 → ACNP
Volume
49
Issue
1-4
Year of publication
2001
Pages
129 - 149
Database
ISI
SICI code
0079-6611(2001)49:1-4<129:TVILTL>2.0.ZU;2-Y
Abstract
An examination of large archives (1950-1997) of the oceanographic and atmos pheric data from the northwestern North Pacific Subtropical Gyre has reveal ed clear linkages between atmospheric forcing factors, physical processes a nd biological events. Large changes in the winter and spring biomass of phy toplankton and macroplankton observed over annual, decadal and inter-decada l time scales could clearly be attributed to climate-related changes in oce anographic processes. Interannual changes in the intensity of the winter-ti me East Asian Monsoon had a significant impact on the extent of convective overturning, on nitrate inputs into the euphotic zone and the concentration s of chlorophyll a in winter and during the following spring. A prolonged p eriod of deeper winter mixed layers observed from the mid-1970s to the mid- 1980s led to a sizeable increase in winter mixed-layer nitrate concentratio ns. This change resulted in a decrease in winter-time phytoplankton biomass . Spring-time chlorophyll a, in contrast, showed a steady increase during t his period. The decline in winter phytoplankton biomass could be attributed to the depths of mixed layer. A deeper mixed layer prevents phytoplankton from remaining in the euphotic zone for long enough to photosynthesize and grow, leaving substantial amounts of nutrients unutilised. However, as a re sult of stratification of the water column in spring following each of thes e winters, phytoplankton could take advantage of the enhanced ambient conce ntrations of nutrients and increase its biomass. Another noteworthy observa tion for the period from the mid- 1970s to the early 1980s is that the west ern subtropical gyre progressively became phosphate limited. The period of diminishing mixed-layer phosphate concentrations was observed in our study area from the early 1990s onwards was consistent with recent observations a t Station ALOHA in the eastern subtropical gyre. (C) 2001 Elsevier Science Ltd. All rights reserved.