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Ch 6 - Earth and Space The Hydrosphere
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Hydrosphere The hydrosphere is the part of the Earth that contains water in all its states: liquid, solid, and gas Lakes, rivers, oceans, glaciers, etc. 97.5% of all water is salt water 2.5% of all water is fresh water Of this 2.5%, 79% of fresh water is trapped and frozen in glaciers 21% of freshwater is available as lakes, rivers and ground water
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Inland Water Def’n: Bodies of freshwater found on continents. Contains rivers, lakes and groundwater. The study of these different waters is divided into catchment areas or watersheds
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Catchment Area - Watersheds
Def’n: A part of land where all inland waters will drain and flow into the same larger body of water Also called drainage basin
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Pollutants More catchment areas a river has, the more polluted the water can become.
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Aspects which affect a watershed
How easily can water flow across a surface? Topography: natural and artificial features of the area Geology: rocks Climate Vegetation Agriculture
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Cryosphere Def’n: The crysophere consists of all frozen water on the Earth’s surface Pack ice, glaciers, frozen lakes and rivers, snow and permafrost Cryo from Greek meaning icy cold
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Pack Ice Huge slabs of ice floating on water. Smaller, free-floating sheets of ice are called ice floes. Generally found in the Artic Ocean near Russia and around Antartica Content and location: freshwater, floating in water
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Shrinking
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Glaciers A mass of ice on land, formed by compressed snow
Large glaciers are called ice caps or ice sheets Note: 79% of freshwater is contained in glaciers Content and location: freshwater, on land
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Icebergs (enrichment)
A piece of a glacier that has broken off and floats into open water Breaking off: It can melt away or can freeze into pack ice Iceberg flipping over:
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Oceans The study of oceans involves two important parameters: Why?
Water temperature Salinity Why? They influence ocean circulation
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Ocean Circulation The Gulf Stream Explained
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The Ocean Large masses of salt water Two types of currents
Surface currents: driven mostly by wind Subsurface currents (deep currents) aka thermohaline circulation: driven by water density differences due to temperature and water
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Surface Currents About 400 m deep : Gulfstream Wind driven
Affected by rotation of the Earth
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Subsurface Currents – Thermohaline Circurlation
Caused by density of water Huge conveyer belt that connects surface and subsurface Distributes heat around the world
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Water temperature is influenced by:
Latitude Where the ocean is located on the Earth relative to the equator influences the average temperature. Map of surface temperatures. Red = warmer. Blue = cooler Approx °C near the equator Approx °C in temperate zones
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Factors that Affect Ocean Circulation
Subsurface currents are driven by differences in density due to temperature and salinity. Cold water is denser and sinks Warm water is lighter and rises Salt differences Salty water is denser and sinks Less salty water is less dense and rises
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Polar Equator
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Most dense water: Cold and salty Less dense water: Warm and less salty
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Pack Ice + Glaciers? As the ice melts, the water is less salty which makes it less dense. The water will no longer sink to the bottom.
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A) Location 1 will be the most affected, since the flow of water will carry the toxic substance into the lake. B) Location 2 will be only slightly affected, since the current will prevent the toxic substance from accumulating. C) Because of the terrain, only location 3 will be affected. D) Location 4 will be affected the most, since it is downstream from the spill
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