Physical and biological responses to the passage of a winter storm in the coastal and inner shelf waters of the northern Gulf of Mexico
Reference (36)
- et al.
Sediment resuspension by coastal waters: a potential mechanism for nutrient recycling on the ocean's margins
Deep-Sea Research
(1982) - et al.
Albacore tuna catch distributions relative to environmental features observed from satellites
Deep-Sea Research
(1984) - et al.
Biological consequences of hydrographic and atmospheric advection within the Gulf Loop Intrusion
Deep-Sea Research
(1984) - et al.
Zonation and maintenance of copepod populations in the Oregon upwelling zone
Deep-Sea Research
(1979) - et al.
Occasional blooms of phytoplankton during summer in Saanich Inlet, B.C., Canada
Deep-Sea Research
(1977) Wind-driven, near-bottom currents over the west Louisiana inner continental shelf
- et al.
The biological response in the sea to climatic changes
Advances in Marine Biology
(1979) Some effects of patchy food environments on copepods
Limnology and Oceanography
(1977)- et al.
Winter-time distribution and abundance of copepod nauplii in the Northern Gulf of Mexico
Fishery Bulletin U.S.A.
(1988) - et al.
An examination of the frequency and mean conditions surrounding frontal incursions into the Gulf of Mexico and the Caribbean Sea
Monthly Weather Review
(1976)
Methods for chemical analysis of water and wastes
A subsynoptic study of winter cold fronts in Florida
Monthly Weather Review
Oceanic distribution of eggs and larvae of the gulf menhaden
Coastal water mass replacement: its effect on zooplankton dynamics and the predator-prey complex associated with larval capelin (Mallotus villosus)
Canadian Journal of Fisheries and Aquatic Science
Patterns and processes in the time-space scales of plankton distributions
Some aspects of the fate of cold fronts in the Gulf of Mexico
Monthly Weather Review
Summer phytoplankton blooms in Auke Bay, Alaska, driven by wind mixing in the water column
Limnology and Oceanography
Field criteria for survival of anchovy larvae: the relation between inshore chlorophyll maximum layers and for successful first feeding
Fishery Bulletin
Cited by (47)
Atmospheric circulation regimes for prescribed burns along the U.S. Gulf of Mexico coast
2021, Applied GeographyCitation Excerpt :Muller (1977) developed a subjective, manual classification system (i.e., without using PCA or related eigenvector techniques) by examining daily weather maps and grouping them according to pre-conceived circulation types. That approach has been applied extensively in the study region over the years (e.g., Dagg, 1988; Engle et al., 2008; Keim & Muller, 1992; Muller & Jackson, 1985; Wang, Ransibrahmanakul, Tuen, Wang, & Zhang, 1995). Lewis and Keim (2015) developed a “hybrid” (i.e., part-subjective and part-objective; Frakes & Yarnal, 1997) approach by conducting correlation-based automated classification of daily weather types based on “key days” that represent prototypes of each of Muller’s (1977) eight categories.
Anomalous summer-autumn phytoplankton bloom in 2015 in the Black Sea caused by several strong wind events
2019, Journal of Marine SystemsCitation Excerpt :Several authors have shown that the maximal response of phytoplankton blooms to typhoons is observed in the subsurface layers (Naik et al., 2008), where nutrients are effectively transported from the deeper layers due to wind-induced upwelling (Ye et al., 2013). Strong winds provide a similar effect, increasing the amount of nitrates (Iverson et al., 1974) and biological productivity (Dagg, 1988; Wu et al., 2008; Zhang et al., 2014) at the sea subsurface. Using Bio-Argo measurements in the Bay of Bengal, Chacko (2017) have recently shown that the action of tropical cyclones induced strong diapycnal fluxes, impacting the ocean thermohaline structure.
Geographic expansion of hermatypic and ahermatypic corals in the Gulf of Mexico, and implications for dispersal and recruitment
2012, Journal of Experimental Marine Biology and EcologyCitation Excerpt :The center of the GOM receives warm water from the Caribbean Current (Oey et al., 2005). During the winter, temperatures on the shelf and in inshore waters reach temperatures as low as 14 °C (Dagg, 1988), outside of the known temperature tolerance range of most hermatypic corals. The extension of hermatypic coral species diversity and density shoreward in Transect 2, south of Lake Sabine, TX, lends support to a hypothesis regarding larval dispersal in the region proposed by Lugo-Fernandez et al. (2001).
Dissolved and colloidal trace elements in the Mississippi River delta outflow after Hurricanes Katrina and Rita
2012, Continental Shelf ResearchCitation Excerpt :With a longer timescale for mixing in the waters of the Louisiana Shelf west of the Delta, dilution of nitrate by mixing becomes a slower process than biological removal (Shiller, 1993b). Additionally, it is likely that passage of the storms resulted in upwelling of low-nitrate shelf bottom water, similar to what was observed by Dagg (1988) in this region following passage of a winter storm. Ammonium, while more scattered, follows a similar trend to nitrate (Fig. 2).
Transformation of dissolved and particulate materials on continental shelves influenced by large rivers: Plume processes
2004, Continental Shelf ResearchLarge-scale environmental influences on the benthic macroinfauna of the southern Gulf of Mexico
2003, Estuarine, Coastal and Shelf Science