{"id":5589,"date":"2020-01-13T22:43:16","date_gmt":"2020-01-13T22:43:16","guid":{"rendered":"https:\/\/course.oeru.org\/eths101\/?page_id=5589"},"modified":"2020-01-13T22:43:16","modified_gmt":"2020-01-13T22:43:16","slug":"hydrosphere","status":"publish","type":"page","link":"https:\/\/course.oeru.org\/eths101\/learning-pathways\/earth-systems\/hydrosphere\/","title":{"rendered":"Hydrosphere"},"content":{"rendered":"<div id=\"content\" class=\"mw-body container\" role=\"main\">\n<div class=\"row\">\n<div class=\"col-md-12\">\n<div class=\"panel\">\n<div class=\"panel-body\">\n<div id=\"bodyContent\">\n<div id=\"mw-content-text\" lang=\"en\" dir=\"ltr\" class=\"mw-content-ltr\">\n<div class=\"floatright\"><a href=\"https:\/\/wikieducator.org\/File:The_Blue_Marble.jpg\" class=\"image\" title=\"Google Earth image\"><img loading=\"lazy\" decoding=\"async\" alt=\"Google Earth image\" src=\"\/\/wikieducator.org\/images\/thumb\/7\/78\/The_Blue_Marble.jpg\/320px-The_Blue_Marble.jpg\" width=\"320\" height=\"320\" class=\"img-responsive\"><\/a><\/div>\n<p> From the darkness of space our planet is blue. This is because it has a hydrosphere and atmosphere. These outer shells surround the geosphere. In this learning pathway, we will find out about these important Earth systems.<br style=\"clear:both\"><\/p>\n<p>In the infographic, on the water cycle (below), you can see the main elements of the water cycle, which involves the geosphere, the hydrosphere, and the atmosphere. Although H2O is mainly liquid, it can also be a gas in the atmosphere or a solid (ice) in the atmosphere, mountain tops, or ice caps.\n<\/p>\n<div class=\"center\">\n<div class=\"floatnone\"><a href=\"https:\/\/wikieducator.org\/File:Water_cycle.png\" class=\"image\" title=\"Water Cycle\"><img loading=\"lazy\" decoding=\"async\" alt=\"Water Cycle\" src=\"\/\/wikieducator.org\/images\/thumb\/9\/94\/Water_cycle.png\/620px-Water_cycle.png\" width=\"620\" height=\"425\" class=\"img-responsive\"><\/a><\/div>\n<\/div>\n<p>\n<\/p>\n<h2><span class=\"mw-headline\" id=\"The_water_cycle\">The water cycle<\/span><\/h2>\n<p>The infographic indicating <b>where is Earth&#8217;s water<\/b> tells us where the water is stored on Earth and in what form. Note that most of the water is in the liquid state in the world&#8217;s oceans and seas and is salty. Freshwater is only 3% of all the Earth&#8217;s water, and most of that is in the form of ice.\n<\/p>\n<div class=\"center\">\n<div class=\"thumb tnone\">\n<div class=\"thumbinner thumbnail\" style=\"width:602px\"><a href=\"https:\/\/wikieducator.org\/File:Earth%27s_water_distribution.svg.png\" class=\"image\"><img loading=\"lazy\" decoding=\"async\" alt=\"\" src=\"\/\/wikieducator.org\/images\/thumb\/d\/dc\/Earth%27s_water_distribution.svg.png\/600px-Earth%27s_water_distribution.svg.png\" width=\"600\" height=\"488\" class=\"thumbimage img-responsive\"><\/a>  <\/p>\n<div class=\"thumbcaption\">Earths water distribution<\/div>\n<\/div>\n<\/div>\n<\/div>\n<p>\n<\/p>\n<div class=\"panel iDevice WEquizMultipleChoice\">\n\t<div class=\"panel-heading idevice-heading\">\n\t\t<div>\n\t\t\t<img decoding=\"async\" class=\"pedagogicalicon\" alt=\"assessment\" src=\"https:\/\/course.oeru.org\/eths101\/wp-content\/themes\/oeru_course\/idevices\/Icon_qmark.png\">\n\t\t<\/div>\n\t\t<div>\n\t\t\t<h2>Quick quiz<\/h2>\n\t\t<\/div>\n\t<\/div>\n\t<div class=\"panel-body\">\n\t\t<div class=\"col-md-12\">\n\t\t\t\n<p>Review the following table summarising the earth&#8217;s water reservoir and answer the question which follows.\n<\/p>\n<table class=\"oeru1 table table-striped\">\n<tbody>\n<tr>\n<th>Reservoir<\/th>\n<th> Residence Time (average)<\/th>\n<\/tr>\n<tr>\n<td>Ocean<\/td>\n<td>3,000 to 3,230 years<\/td>\n<\/tr>\n<tr>\n<td>Glaciers<\/td>\n<td>20 to 100 years<\/td>\n<\/tr>\n<tr>\n<td>Seansonal Snow Cover<\/td>\n<td>2 to 6 Months<\/td>\n<\/tr>\n<tr>\n<\/tr>\n<tr>\n<td>Soil Moisture<\/td>\n<td>1 to 2 months<\/td>\n<\/tr>\n<tr>\n<td>Groundwater: Shallow<\/td>\n<td>100 to 200 years<\/td>\n<\/tr>\n<tr>\n<td>Groundwater:Deep <\/td>\n<td>10,000 years<\/td>\n<\/tr>\n<tr>\n<td>Lakes<\/td>\n<td>50 to 100 years<\/td>\n<\/tr>\n<tr>\n<td>Rivers<\/td>\n<td>2 to 6 Months<\/td>\n<\/tr>\n<tr>\n<td>Atmosphere<\/td>\n<td>6 days<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<ul>\n<li> Which water reservoir holds its water the longest?\n<ul>\n<li> The atmosphere\n<ul>\n<li> <b>Incorrect<\/b>.  Review the table above OR think a little &#8220;lower&#8221;.\n<\/li>\n<\/ul>\n<\/li>\n<li> The ocean\n<ul>\n<li> <b>Incorrect<\/b>. Review the table above .\n<\/li>\n<\/ul>\n<\/li>\n<li> Groundwater\n<ul>\n<li> <b>Correct<\/b>.  <big><b>If you thought the answer was Ground Water you were correct. In some areas of the Great Artesian Basin that spreads west of Australia&#8217;s Great Dividing Range into the dry inland, groundwater extracted can be millions of years old.<\/b><\/big>\n<\/li>\n<\/ul>\n<\/li>\n<li> Lakes\n<ul>\n<li> <b>Incorrect<\/b>.  Review the table above.\n<\/li>\n<\/ul>\n<\/li>\n<li>They all hold water for the same amount of time.\n<ul>\n<li> <b>Incorrect<\/b>. There is a better answer available to you, try again.\n<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>\n<\/p>\n<p>\n\t\t<\/div>\n\t<\/div>\n<\/div><\/p>\n<p>\n<\/p>\n<p>\n<\/p>\n<div class=\"panel iDevice WEquizMultipleChoice\">\n\t<div class=\"panel-heading idevice-heading\">\n\t\t<div>\n\t\t\t<img decoding=\"async\" class=\"pedagogicalicon\" alt=\"assessment\" src=\"https:\/\/course.oeru.org\/eths101\/wp-content\/themes\/oeru_course\/idevices\/Icon_qmark.png\">\n\t\t<\/div>\n\t\t<div>\n\t\t\t<h2>Does more water evaporate from the ocean, or from the land?<\/h2>\n\t\t<\/div>\n\t<\/div>\n\t<div class=\"panel-body\">\n\t\t<div class=\"col-md-12\">\n\t\t\t\n<table class=\"oeru1 table table-striped\">\n<tbody>\n<tr>\n<th>Process<\/th>\n<th> From and <b>to<\/b> which Reservoir<\/th>\n<th> Flow Rate  (km cubed)<\/th>\n<\/tr>\n<tr>\n<td>Precipitation<\/td>\n<td>Atmosphere <b>to<\/b> Ocean &amp; Land<\/td>\n<td>505,00km\/year<\/td>\n<\/tr>\n<tr>\n<td>Ocean Precipitation<\/td>\n<td>Atmosphere <b>to<\/b> Ocean<\/td>\n<td>398,000km\/year<\/td>\n<\/tr>\n<tr>\n<td>land Precipitation (exept snow)<\/td>\n<td>Atmosphere <b>to<\/b> Land and Surface<\/td>\n<td>96,000 to 107,000km\/year<\/td>\n<\/tr>\n<tr>\n<\/tr>\n<tr>\n<td>Eavotranspiration<\/td>\n<td>Ocean &amp; Land <b>to<\/b> surface &amp; Plants <b>to<\/b> Atmosphere<\/td>\n<td>505,000km\/year<\/td>\n<\/tr>\n<tr>\n<td>Ocean Evaporation<\/td>\n<td>Ocean <b>to<\/b> Atmosphere<\/td>\n<td>434,000km\/year<\/td>\n<\/tr>\n<tr>\n<td>Land evaporation<\/td>\n<td>Land &amp; Surface <b>to<\/b> Atomsphere<\/td>\n<td>50,000km\/year<\/td>\n<\/tr>\n<tr>\n<td>Transpiration <\/td>\n<td>Plants <b>to<\/b> Atmosphere<\/td>\n<td>21,000km\/year<\/td>\n<\/tr>\n<tr>\n<td>Uptake by plants<\/td>\n<td>Land &amp; surface <b>to<\/b> Biota<\/td>\n<td>21,000km\/year<\/td>\n<\/tr>\n<tr>\n<td>Runoff<\/td>\n<td>Land and Surface <b>to<\/b> Ocean<\/td>\n<td>36,000km\/year<\/td>\n<\/tr>\n<tr>\n<td>Melting<\/td>\n<td>Ice &amp; Snow <b>to<\/b> Land &amp; Surface<\/td>\n<td>11,000km\/year<\/td>\n<\/tr>\n<tr>\n<td>Snowfall (on Land)<\/td>\n<td>Atmosphere <b>to<\/b> Ice &amp; Snow<\/td>\n<td>11,000km\/year<\/td>\n<\/tr>\n<tr>\n<td>Percolation<\/td>\n<td>Underground to and from Land<\/td>\n<td>100km\/year<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<p>\n<\/p>\n<ul>\n<li> Select one from the below\n<ul>\n<li> The Ocean\n<ul>\n<li> <b>Correct<\/b>.  Well done, there is a significant difference between the two, which leads us to the question below.\n<\/li>\n<\/ul>\n<\/li>\n<li> The Land\n<ul>\n<li> <b>Incorrect<\/b>. Consider using the table to your right.\n<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>\n<\/p>\n<p>\n\t\t<\/div>\n\t<\/div>\n<\/div><\/p>\n<p>\n<\/p>\n<p>\n<\/p>\n<div class=\"thumb tright\">\n<div class=\"thumbinner thumbnail\" style=\"width:322px\"><a href=\"https:\/\/wikieducator.org\/File:Ocean-waves-background-1524840234EgG.jpg\" class=\"image\"><img loading=\"lazy\" decoding=\"async\" alt=\"\" src=\"\/\/wikieducator.org\/images\/thumb\/e\/ef\/Ocean-waves-background-1524840234EgG.jpg\/320px-Ocean-waves-background-1524840234EgG.jpg\" width=\"320\" height=\"195\" class=\"thumbimage img-responsive\"><\/a>  <\/p>\n<div class=\"thumbcaption\">Ocean Waves<\/div>\n<\/div>\n<\/div>\n<p>If more water is <b>evaporating<\/b> from the ocean than <b>precipitating<\/b> into the ocean, how come we are worried about sea level rise?\n<\/p>\n<p>Share your thoughts on the WeNote pannel below. We encourage you to share your thought, however, if you are stuck you can find the answer to this question at the bottom of this learning page.\n<\/p>\n<ul>\n<li> Ocean precipitation = 398,000 km3\/year\n<\/li>\n<li> Ocean evaporation = 434,000 km3\/year\n<\/li>\n<\/ul>\n<div><p>You must be logged in to post to WEnotes.<\/p><\/div>\n<p><i>Note: Your comment will be displayed in the <a href=\"\/eths101\/interactions\/course-feed\" title=\"Human earth shapers\/ETHS101\/Feed\">course feed<\/a>.<\/i>\n<\/p>\n<p>\n<br style=\"clear:both\">\n<\/p>\n<div class=\"panel iDevice WEquizMultipleChoice\">\n\t<div class=\"panel-heading idevice-heading\">\n\t\t<div>\n\t\t\t<img decoding=\"async\" class=\"pedagogicalicon\" alt=\"assessment\" src=\"https:\/\/course.oeru.org\/eths101\/wp-content\/themes\/oeru_course\/idevices\/Icon_qmark.png\">\n\t\t<\/div>\n\t\t<div>\n\t\t\t<h2>Sea Level: Contributors<\/h2>\n\t\t<\/div>\n\t<\/div>\n\t<div class=\"panel-body\">\n\t\t<div class=\"col-md-12\">\n\t\t\t\n<p>Match the explanation with the correct term\n<\/p>\n<ul>\n<li> Isostatic change occurs when the mass of continents increases or decreases due to the buildup of ice and snow. This process happens on geological timeframes while glaciers build up at the onset of ice ages (increasing the mass of continents), and melt as ice ages end (decreases the mass of continents). When the continent&#8217;s increase in mass, land sinks deeper into the ocean, increasing sea levels.\n<ul>\n<li> Warming of oceans\n<ul>\n<li> <b>Incorrect<\/b>.  Unlucky, try again.\n<\/li>\n<\/ul>\n<\/li>\n<li> Changes in Land Masses\n<ul>\n<li> <b>Correct<\/b>.\n<\/li>\n<\/ul>\n<\/li>\n<li> Melting Icebergs\n<ul>\n<li> <b>Incorrect<\/b>.  Unlucky, try again.\n<\/li>\n<\/ul>\n<\/li>\n<li> Melting Ice Caps\n<ul>\n<li> <b>Incorrect<\/b>. Unlucky, try again\n<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<\/li>\n<li> When the oceans warm, water molecules take up more space, increasing the volume of the ocean. This is called thermal expansion\n<ul>\n<li> Melting Icebergs\n<ul>\n<li> <b>Incorrect<\/b>.  Try Again.\n<\/li>\n<\/ul>\n<\/li>\n<li> Melting Ice Caps\n<ul>\n<li> <b>Incorrect<\/b>. Try again\n<\/li>\n<\/ul>\n<\/li>\n<li> Changing land Masses\n<ul>\n<li> <b>Incorrect<\/b>.  Try again.\n<\/li>\n<\/ul>\n<\/li>\n<li> Warming Oceans\n<ul>\n<li> <b>Correct<\/b>. Well Done.\n<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<\/li>\n<li> as global temperatures rise, ice caps melt and the runoff flows into the oceans. This shouldn&#8217;t be confused with melting Icebergs, although some fraction of an iceberg is above the surface, the volume of liquid water is smaller than the volume of frozen water for the same number of molecules, therefore, ice already floating in the ocean has a negligible effect on sea levels.\n<ul>\n<li> Melting Icebergs\n<ul>\n<li> <b>Incorrect<\/b>.  Try Again.\n<\/li>\n<\/ul>\n<\/li>\n<li> Melting Ice Caps\n<ul>\n<li> <b>Correct<\/b>. Well Done.\n<\/li>\n<\/ul>\n<\/li>\n<li> Changing land Masses\n<ul>\n<li> <b>Incorrect<\/b>.  Try again.\n<\/li>\n<\/ul>\n<\/li>\n<li> Warming Oceans\n<ul>\n<li> <b>Incorrect<\/b>.  try again\n<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>\n<\/p>\n<p>\n\t\t<\/div>\n\t<\/div>\n<\/div><\/p>\n<p>\n<\/p>\n<p>\n<br style=\"clear:both\">\n<\/p>\n<h2><span class=\"mw-headline\" id=\"Water_-_Unique_characteristics_that_make_water_what_it_is.\">Water &#8211; Unique characteristics that make water what it is.<\/span><\/h2>\n<p>In this section, we consider the unique properties of water, and how these affect global temperature, weather and climate.\n<\/p>\n<h3><span class=\"mw-headline\" id=\"Unusual_Properties_of_Water\">Unusual Properties of Water<\/span><\/h3>\n<table class=\"oeru1 table table-striped\">\n<tbody>\n<tr>\n<td>High boiling point<\/td>\n<td>High melting point<\/td>\n<td>High specific heat<\/td>\n<\/tr>\n<tr>\n<td>High heat conductivity<\/td>\n<td>High heat of evaporation<\/td>\n<td>High heat of freezing<\/td>\n<\/tr>\n<tr>\n<td>Maximum density at 4\u00b0C (pure water)<\/td>\n<td>High surface tension<\/td>\n<td>High viscosity<\/td>\n<\/tr>\n<tr>\n<td>High dielectric constant<\/td>\n<td><\/td>\n<td><\/td>\n<\/tr>\n<tr>\n<\/tr>\n<\/tbody>\n<\/table>\n<h3><span class=\"mw-headline\" id=\"How_do_these_unique_properties_of_water_affect_global_temperatures.3F\">How do these unique properties of water affect global temperatures?<\/span><\/h3>\n<dl>\n<dd>\n<ul>\n<li>The oceans can hold a lot of energy without changing temperature \u2013 thermal inertia\n<\/li>\n<li>Important vehicle for heat and energy transfer between the oceans and atmosphere\n<\/li>\n<li>Transfers energy from the equator to the poles\n<\/li>\n<li>Thawing and freezing of ice at the poles moderates global temperatures, absorbing and releasing energy without changing ocean temperatures\n<\/li>\n<\/ul>\n<\/dd>\n<\/dl>\n<h3><span class=\"mw-headline\" id=\"What_about_ocean_circulation.3F_How_does_that_affect_weather_and_climate.3F\">What about ocean circulation? How does that affect weather and climate?<\/span><\/h3>\n<dl>\n<dd>\n<ul>\n<li>Ocean circulation can be divided into surface and deep currents\n<\/li>\n<li>The surface currents are driven by the winds, by the rotation of the earth, and by differences in seawater density, which cause differences in the height of the sea surface\n<\/li>\n<li>Deep ocean circulation, also known as the thermohaline (thermo = temperature, haline = salt) circulation, is driven by density differences, caused by differences in temperature and salinity\n<\/li>\n<li>Both deep ocean and surface ocean circulation move heat, gases, and nutrients around the planet, and play a key role in climate and weather\n<\/li>\n<li>Learn more by <a rel=\"nofollow\" class=\"external text\" href=\"https:\/\/www.nationalgeographic.org\/media\/ocean-currents-and-climate\/\">watching this short video on the deep ocean circulation and its role in climate<\/a>\n<\/li>\n<\/ul>\n<\/dd>\n<\/dl>\n<p>\n<\/p>\n<div class=\"container\">\n<h2><span class=\"mw-headline\" id=\"Summary\">Summary<\/span><\/h2>\n<div class=\"panel panel-default\">\n<div class=\"panel-body\">Now that you know some interesting things about the hydrosphere have a look at the next page on the atmosphere.<\/div>\n<\/p><\/div>\n<\/div>\n<p><b>WeNote Activity<\/b>: If more water is <b>evaporating<\/b> from the ocean than <b>precipitating<\/b> into the ocean, how come we are worried about sea level rise?\n<\/p>\n<ul>\n<li><b>Answer<\/b>: Although more water evaporates from the ocean, river runoff from the continents into the ocean make up the balance.\n<\/li>\n<\/ul>\n<p><!-- \nNewPP limit report\nCPU time usage: 0.303 seconds\nReal time usage: 2.071 seconds\nPreprocessor visited node count: 417\/1000000\nPreprocessor generated node count: 1320\/1000000\nPost\u2010expand include size: 27118\/2097152 bytes\nTemplate argument size: 20102\/2097152 bytes\nHighest expansion depth: 8\/40\nExpensive parser function count: 0\/100\n--><\/p>\n<p><!-- Saved in parser cache with key we_en-mw_:pcache:idhash:184991-0!*!0!!en!2!* and timestamp 20200113224312 and revision id 1064124\n -->\n<\/div>\n<div class=\"visualClear\"><\/div>\n<\/p><\/div>\n<\/p><\/div>\n<\/div>\n<\/div>\n<\/div>\n<div class=\"row\">\n<div class=\"col-md-12\">\n<ul class=\"pager\">\n<li class=\"previous\">\n            <a href=\"\/eths101\/learning-pathways\/earth-systems\/geosphere\">\u2190 Previous<\/a>\n          <\/li>\n<li class=\"next\">\n            <a href=\"\/eths101\/learning-pathways\/earth-systems\/atmosphere\">Next \u2192<\/a>\n          <\/li>\n<\/ul><\/div>\n<\/p><\/div>\n<\/div>\n<footer>\n<br \/>\n<\/footer>\n","protected":false},"excerpt":{"rendered":"<p>From the darkness of space our planet is blue. This is because it has a hydrosphere and atmosphere. These outer shells surround the geosphere. In this learning pathway, we will find out about these important Earth systems. In the infographic, on the water cycle (below), you can see the main elements of the water cycle, [&hellip;]<\/p>\n","protected":false},"author":155,"featured_media":0,"parent":5583,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-5589","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/course.oeru.org\/eths101\/wp-json\/wp\/v2\/pages\/5589","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/course.oeru.org\/eths101\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/course.oeru.org\/eths101\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/course.oeru.org\/eths101\/wp-json\/wp\/v2\/users\/155"}],"replies":[{"embeddable":true,"href":"https:\/\/course.oeru.org\/eths101\/wp-json\/wp\/v2\/comments?post=5589"}],"version-history":[{"count":1,"href":"https:\/\/course.oeru.org\/eths101\/wp-json\/wp\/v2\/pages\/5589\/revisions"}],"predecessor-version":[{"id":5590,"href":"https:\/\/course.oeru.org\/eths101\/wp-json\/wp\/v2\/pages\/5589\/revisions\/5590"}],"up":[{"embeddable":true,"href":"https:\/\/course.oeru.org\/eths101\/wp-json\/wp\/v2\/pages\/5583"}],"wp:attachment":[{"href":"https:\/\/course.oeru.org\/eths101\/wp-json\/wp\/v2\/media?parent=5589"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}