UNIT 7 – OCEANS AND CLIMATE CH 15 Ocean Water and Ocean Life 15.1 The Composition of Seawater Salinity Salinity is the amount of solid material dissolved in water. It is expressed in __________ per __________________ which is abbreviated _____________. The average salinity of seawater is _______________. Most of the salt in seawater is ___________ ______________, common table salt. The salt comes from ________________ ______________ of rocks on the continents. The second major source of elements found in seawater is from Earth’s ______________________. Processes Affecting Salinity Processes that Decrease Salinity o __________________________________________________________ o __________________________________________________________ o __________________________________________________________ o __________________________________________________________ Processes that increase salinity o __________________________________________________________ o __________________________________________________________ Ocean Temperature Variation The ocean’s surface water temp varies with ________________________________________________________ which is primarily a function of latitude. Temperature Variation with Depth The _____________________________ is the layer of the ocean water between about 300m and 1000m where there is a rapid change in temp. The ______________________________ is a very important structure because it creates a barrier to marine life. Ocean Density Variation Density is defined as _____________________ per unit ______________________. Factors Affecting Seawater Density -------------------------------------------------_______________________________ The __________________________ is the layer of ocean water between about 300m and 1000m where there is a rapid change of density with depth. Ocean Layering Mainly a 3 layer structure in ocean: 1. ___________________ ___________ - shallow (300-450m), zone of mixing, sun-warmed zone 2. ____________________ _____________ - between surface layer and deep zone, thermocline and pyncocline 3. ______________ _____________ - sunlight never reaches this zone, temps just a few degrees above freezing, constant high-density water CH 16 The Dynamic Ocean 16.1 Ocean Circulation Surface Circulation __________ _______________ is the mass of ocean water that flows from one place to another. Surface Currents Surface currents are ______________ of _________________ that flow ________________________ in the __________ part of the ocean’s ________________. Surface currents develop from _____________ between the ocean and the _________ that blows across its surface. Surface Circulation Gyres o Gyres are huge circular-moving current systems that dominate the surfaces of the oceans. o The _________________ ________________ is the deflection of currents away from their original course as a result of _________________ __________________. In the northern hemisphere, currents deflect to the ________________. Ocean Currents and Climate o When currents from low-latitude regions move into higher latitudes, the transfer _________ from warmer to cooler areas on Earth. o As cold water currents travel toward the ______________, they help moderate the warm temperatures of adjacent land areas. Upwelling o Upwelling is the rise of ________ ___________ from deeper layers to replace warmer surface water. o Upwelling brings greater concentrations of ________________ _____________, such as nitrates and phosphates to the surface. Deep-Ocean Circulation Density Currents o Density currents are ______________ currents of ocean water that result from the ____________ differences among water masses. o An increase in seawater density can be caused by a __________ in ___________________ or an ______________ in _________________. High Latitudes – most water involved in deep-ocean currents begins in high latitudes at the surface Evaporation – density currents can also result from _____________ _____________ of ocean water due to evaporation A Conveyor Belt – ocean circulation is similar to a conveyor belt that travels from the ______________ _________ through the ____________ and ______________ ____________ and back again. 16.2 Waves and Tides Wave Characteristics o Most ocean waves obtain their energy and motion from the ___________. o __________ _______________ is the vertical distance between the trough and crest. o _______________________ is the horizontal distance between two successive troughs. o ______________ ________________ is the time it takes one full wave – one wavelength – to pass a fixed position. o ________ is the distance that the wind has traveled across open water. o The height, length and period that are eventually achieved by a wave depend on 3 factors: ____________________, _______________________________________________________ and ____________. Wave Motion o ______________ ______________ motion allows energy to move forward through the water while while the individual water particles that transmit the wave move around in a __________. Breaking Waves o Changes occur as a wave moves onto shore o As the wave touches the bottom, wave speed ______________. The decrease in wave speed results in a _________________ in wavelength and an _______________ in wave height. Tides __________ are daily changes in the elevation of the ocean surface. Ocean tides result from the __________________ __________________ exerted upon Earth by the ______ and, to a lesser extent, by the ________. Tide-causing Forces o The force that produces tides is _____________________. Tidal Cycle o _________ ________ is the difference in height between successive high and low tides. o _____________ ___________ are tides that have the greatest tidal range due to the alignment of the Earth-moon-sun system. o __________ _____________ are tides that have the lowest tidal range, occurring near the times of the first-quarter and third-quarter phases of the moon. Tidal Patterns o 3 main tidal patterns exist worldwide: ______________________________, _________________________, and ______________________________________.