@article {262,
	title = {Intra-seasonal and inter-annual variations in phytoplankton biomass, primary production and bacterial production at North West Cape, Western Australia: Links to the 1997{\textendash}1998 El Ni{\~n}o event},
	journal = {Continental Shelf Research},
	volume = {27},
	year = {2007},
	month = {04/2007},
	pages = {958-980},
	abstract = {Phytoplankton biomass, community and size structure, primary production and bacterial production were measured at shelf and continental slope sites near North West Cape, Western Australia (20.5{\textdegree}S{\textendash}22.5{\textdegree}S) over two summers (October{\textendash}February 1997{\textendash}1998 and 1998{\textendash}1999), and in April 2002. The North West Cape region is characterized by upwelling-favorable, southwesterly winds throughout the summer. Surface outcropping of upwelled water is suppressed by the geostrophic pressure gradients and warm low-density surface waters of the southward flowing Leeuwin Current. Strong El Ni{\~n}o (ENSO) conditions (SOI <0) prevailed through the summer of 1997{\textendash}1998 which resulted in lower sea levels along the northwestern Australian coast and a weaker Leeuwin Current. La Ni{\~n}a conditions prevailed during the 1998{\textendash}1999 summer and in April 2002. During the summer of 1997{\textendash}1998, the North West Cape region was characterized by a shallower thermocline (nutricline), resulting in larger euphotic zone stocks of inorganic nitrogen and silicate over the continental slope. There was evidence for episodic intrusions of upper thermocline waters and the sub-surface chlorophyll maximum onto the outer continental shelf in 1997{\textendash}1998, but not in 1998{\textendash}1999. Pronounced differences in phytoplankton biomass, community size structure and productivity were observed between the summers of 1997{\textendash}1998 and 1998{\textendash}1999 despite general similarities in irradiance, temperature and wind stress. Phytoplankton primary production and bacterial production were 2- to 4-fold higher during the summer of 1997{\textendash}1998 than in 1998{\textendash}1999, while total phytoplankton standing crop increased by<2-fold. Larger phytoplankton (chiefly diatoms in the >10 μm size fraction) made significant contributions to phytoplankton standing crop and primary production during the summer of 1997{\textendash}1998, but not 1998{\textendash}1999. Although there were no surface signs of upwelling, primary production rates near North West Cape episodically reached levels (3{\textendash}8 g C m-2 day-1) characteristic of eastern boundary Ekman upwelling zones elsewhere in the world. Bacterial production (0.006{\textendash}1.2 g C m-2 day-1) ranged between 0.6 and 145 percent (median=19 percent) of concurrent primary production. The observed differences between years and within individual summers suggest that variations in the Leeuwin Current driven by seasonal or ENSO-related changes in the Indonesian throughflow region may have episodic, but significant influences on pelagic productivity along the western margin of Australia.},
	keywords = {Ningaloo, oceanography, plankton, upwelling},
	doi = {10.1016/j.csr.2007.01.002},
	url = {http://www.sciencedirect.com/science/article/pii/S0278434307000167},
	author = {Furnas, M}
}
