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Time-series analysis of remote-sensed chlorophyll and environmental factors in the Santa Monica-San Pedro Basin off Southern California Nezlin, N.P.; Li, B.-L. (2003). Time-series analysis of remote-sensed chlorophyll and environmental factors in the Santa Monica-San Pedro Basin off Southern California. J. Mar. Syst. 39(3-4): 185-202. https://dx.doi.org/10.1016/S0924-7963(03)00030-7 In: Journal of Marine Systems. Elsevier: Tokyo; Oxford; New York; Amsterdam. ISSN 0924-7963; e-ISSN 1879-1573, meer

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Beschikbaar in	Auteurs
VLIZ: Non-open access 352414 [ aanvragen ]

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Trefwoorden

Analysis > Mathematical analysis > Statistical analysis > Time series analysis Chemical compounds > Organic compounds > Carbohydrates > Glycosides > Pigments > Photosynthetic pigments Environmental conditions INE, USA, California, Southern California Bight Remote sensing Marien/Kust

Author keywords

remote sensing; photosynthetic pigments; environmental conditions;time-series analysis; USA; California; Southern California Bight;33-34.5 degrees N; 119-118 degrees W

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Auteurs		Top
Nezlin, N.P. Li, B.-L.

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Abstract

The time-series of remote-sensed surface chlorophyll concentration measured by SeaWiFS radiometer from September 1997 to December 2001 and the relevant hydrological and meteorological factors (remote-sensed sea surface temperature, atmospheric precipitation, air temperature and wind stress) in Santa Monica Bay and adjacent waters off southern California were analyzed using wavelet and cross-correlation statistical methods. All parameters exhibited evident seasonal patterns of variation. Wavelet analysis revealed salient long-term variations most evident in air temperature during El Niño 1997–1998 and in wind stress during La Niña 1998–1999. Short-period (<100 days) variations of remote-sensed chlorophyll biomass were mostly typical to spring seasons. Chlorophyll biomass was significantly correlated with air temperature and wind stress: an increase of chlorophyll biomass followed with 5–6-day time lag an increase of wind stress accompanied by a simultaneous decrease of air temperature. The mechanism of these variations was an intensification of phytoplankton growth resulting from the mixing of water column by wind stress and entrainment of nutrients into the euphotic layer.

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