Hydrography and plankton temporal variabilities at different time scales in the southwest lagoon of New Caledonia: A review

• Published in: Marine pollution bulletin Vol. 61; no. 7-12; pp. 297 - 308
• Main Authors: Le Borgne, Robert, Douillet, Pascal, Fichez, Renaud, Torréton, Jean-Pascal
• Format: Journal Article
• Language: English
• Published: England Elsevier Ltd 01.01.2010; Elsevier
• Subjects: Coral reef lagoon; Earth Sciences; Ecosystem; Hydrography; Marine; Meteorology; New Caledonia; Oceanography; Plankton; Plankton - physiology; Sciences of the Universe; Seasons; Seawater - chemistry; Temperature; Temporal variability; Time Factors; Water Movements; New Caledonia; ISEW, Pacific, New Caledonia, Noumea; ISEW, Pacific, New Caledonia; Coral reef lagoon; Plankton; Temporal variability; Hydrography; Meteorology; CORAL-REEF LAGOON; SEASONAL-VARIATIONS; PACIFIC; DYNAMICS; WEST LAGOON; BAY; COMMUNITIES; INPUTS
• ISSN: 0025-326X; 1879-3363; 1879-3363
• DOI: 10.1016/j.marpolbul.2010.06.022

The New Caledonia SW lagoon is wide (5–20 nautical miles) and semi-closed. It is influenced by both the open ocean and the high island within a meteorological context subject to seasonal, inter-annual and longer term variations. The short-term variability (>1day) of meteorological, hydrographical and planktonic parameters is illustrated by a 5-month long time series and is linked to local or remote wind, and precipitation. Seasonal and inter-annual variabilities, inferred from a 10-year long station by spectral analysis, appear clearly for all parameters. Seasonality is the main scale of variability as the island lies near the tropic of Capricorn. Inter-annual variability of a 3–4year periodicity is poorly related to the Southern oscillation index (an equatorial climatic index), stressing the need for a separate tropical index. Long term trends appear on several parameters but their reliability depends on the length of the records. Considering only the longest records (1958–2005), surface temperature appears to have increased since the end of the 1960s in Noumea area. Finally, as a result of greater terrestrial influence, shallower depths, and longer water turnover times close to shore, the temporal variability amplitude decreases from the shore to the barrier reef.