Ocean & Coastal Processes Flashcards
(47 cards)
Phytoplankton
Microscopic, photosynthetic organisms that form the base of the marine food web; primary producers in the ocean
Zooplankton
Tiny animal plankton that feed on phytoplankton and serve as food for larger marine animals
Food Web
A complex network of interconnected food chains showing energy transfer between marine organisms
Biomass
The total mass of living organisms in a given area or volume; high near coastlines and upwelling zones due to nutrient availability
Invertebrates
Animals without backbones, such as jellyfish, crustaceans, and corals; make up the majority of marine species
Vertebrates
Animals with backbones, such as fish, whales, and dolphins; often higher up in the marine food web
Bathymetry
The measurement of ocean depth and the mapping of the seafloor; reveals underwater features like trenches, ridges, and continental margins
Continental Margin
The submerged outer edge of a continent, consisting of the continental shelf, slope, and rise
Water Column
A vertical section of ocean water from the surface to the bottom, used to study how light, temperature, and pressure change with depth
Intertidal Zone
The coastal area between high and low tide marks; regularly exposed and submerged
Neritic Zone
The shallow ocean zone over the continental shelf; sunlight reaches the bottom and supports high biodiversity
Oceanic Zone
The deep ocean beyond the continental shelf; includes the photic and aphotic zones
Light/Dark Locations in Water
Horizontal: More light near the coast (neritic), less in deep ocean (oceanic); vertical: light penetrates the photic zone (upper ~200m); aphotic zone lies below where no light reaches
Salinity
The concentration of dissolved salts in water; affects density. Higher salinity = higher density
Water Density, Salinity, Temperature, Pressure
Density increases with salinity and pressure, and decreases with higher temperature. Cold salty water is the densest and sinks during downwelling
Oceanic Heat Transfer
Oceans absorb and redistribute heat via surface currents and deepwater circulation, influencing climate
Surface Currents
Horizontal currents driven by global winds and Earth’s rotation; move warm and cold water across oceans
Global Winds
Include 1) trade winds (near equator, east to west), 2) westerlies (mid-latitudes, west to east), and 3) polar easterlies (poles, east to west)
Coriolis Effect
The deflection of moving fluids (like wind and water) due to Earth’s rotation; causes currents to veer right in the Northern Hemisphere, left in the Southern
Gyres
Large circular current systems in ocean basins, shaped by global winds and the Coriolis effect
Rip Currents
A fast, narrow current moving seaward from the shore; dangerous to swimmers, often formed near breaks in sandbars
Thermohaline Circulation
Global deep-ocean circulation driven by differences in temperature and salinity (density); also called the “global conveyor belt”
Downwelling
Occurs when dense surface water sinks, transporting oxygen to deep waters
Upwelling
Occurs when deep, cold, nutrient-rich water rises to the surface, supporting high biological productivity