{"id":107,"date":"2020-09-29T13:57:16","date_gmt":"2020-09-29T13:57:16","guid":{"rendered":"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/?post_type=chapter&#038;p=107"},"modified":"2020-10-20T16:13:59","modified_gmt":"2020-10-20T16:13:59","slug":"groundwater-flow-at-the-continental-scale","status":"publish","type":"chapter","link":"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/chapter\/groundwater-flow-at-the-continental-scale\/","title":{"raw":"4.4  The Continental Scale View","rendered":"4.4  The Continental Scale View"},"content":{"raw":"Zooming farther out provides an even larger view of the groundwater portion of the hydrologic cycle, extending from the continental divide to the coastal ocean (Figure\u00a035). Broadly, there are two end members of the continental scale system:\r\n<ul>\r\n \t<li>the headwaters in mountainous regions near the continental divide; and,<\/li>\r\n \t<li>the lower basins in flat regions near the coast.<\/li>\r\n<\/ul>\r\nConnecting the headwaters and the lower basins are two, large, continental\u2011scale, terrestrial, water transport systems: one above ground and the other in the subsurface.\r\n<ul>\r\n \t<li>The above ground system is the readily observable stream network, which is concentrated (in channels) and is largely two\u2011dimensional (hugging the land surface). Small upland streams cascade over the surface and converge down\u2011gradient in an orderly manner.<\/li>\r\n \t<li>The subsurface system is the difficult\u2011to\u2011observe groundwater system, which is diffuse (not in channels nor tunnels, except in karst terrain, but rather in pores and fractures of geologic materials), which, relative to the stream network, is three\u2011dimensional (with flow paths that do not necessarily follow the shape of the land surface). Patterns of groundwater flow are less orderly than the stream network because groundwater is driven by multi\u2011scale hydraulic head gradients that are strongly deflected or contorted by complex geologic structures.<a id=\"Figure35\"><\/a><\/li>\r\n<\/ul>\r\n[caption id=\"attachment_202\" align=\"alignnone\" width=\"1024\"]<img class=\"wp-image-202 size-large\" src=\"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig35-1024x793.jpg\" alt=\"Figure showing groundwater flow at the continental scale\" width=\"1024\" height=\"793\" \/> <strong>Figure 35 -<\/strong> The continental view, showing the spatial context of: a) both losing and gaining streams as well as submarine groundwater discharge; and, b) the multi scale nature of groundwater flow systems with shallow, local flow systems nested within deeper intermediate systems which are nested in regional flow systems. This illustrates the long distance hydrologic connectivity of the surface and subsurface water system through exchange between rivers and groundwater, and discharge of rivers and groundwater to the ocean (adapted from Winter et al. 1998).[\/caption]\r\n\r\nWater is exchanged between the surface and subsurface as illustrated by gaining and losing streams and submarine seeps (Figure\u00a035a), and local and regional groundwater flow systems develope (Figure\u00a035b). The <em>local systems tend to be shallow and short<\/em>, and respond to short\u2011term rain events and seasonal changes in climatic conditions. The <em>regional systems are deeper and longer<\/em>. Regional systems tend to \u201crecord\u201d the climate conditions from decades to centuries to millenia ago. For example, a gaining stream in the lower reaches of a basin that is supplied by regional groundwater flow may never run dry, even after long droughts because the groundwater was recharged thousands or tens of thousands years ago when the climate was different.\r\n\r\nAs shown in the large\u2011scale continental view of Figure\u00a035, groundwater can directly discharge into the ocean along the coast of the continent. This is referred to as <em>submarine groundwater discharge<\/em>. Such features were understood and utilized by sea\u2011faring people to locate fresh water long ago as illustrated in Figure\u00a036. Much submarine groundwater discharge occurs close to shore such as in bays and estuaries.\r\n\r\n[caption id=\"attachment_205\" align=\"alignnone\" width=\"864\"]<img class=\"wp-image-205 size-full\" src=\"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig36.jpg\" alt=\"Figure illustrating the use of submarine springs for drinking water by seafarers\" width=\"864\" height=\"572\" \/> <strong>Figure 36 -<\/strong> Submarine springs were correctly understood and utilized for drinking water by seafaring people long ago: a) salt water; b) fresh water; c) low permeability geologic layers; and d) permeable geologic layer. (after Humboldt (1825) who drew the submarine spring diagram as published in the translation by Thrasher in 1856).[\/caption]\r\n\r\nIn summary, there are <strong>three continental\u2011scale water transport systems<\/strong>:\r\n<ol>\r\n \t<li>The <strong>atmosphere<\/strong><strong>;<\/strong><\/li>\r\n \t<li>The <strong>stream networks<\/strong><strong>;<\/strong> and,<\/li>\r\n \t<li>The <strong>groundwater systems<\/strong><strong>. <\/strong><\/li>\r\n<\/ol>\r\nThese continental\u2011scale systems are not isolated. They do not simply deliver continental rainfall back to the ocean in parallel flow systems, rather they are intimately connected and exchange water many times along the way (Figure\u00a037).\r\n\r\n[caption id=\"attachment_207\" align=\"alignnone\" width=\"1024\"]<img class=\"wp-image-207 size-large\" src=\"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig37-1024x566.jpg\" alt=\"Figure showing three continental scale water transport systems\" width=\"1024\" height=\"566\" \/> <strong>Figure 37 -<\/strong> Three continental scale water transport systems: air circulation in the atmosphere, stream networks on surface, and groundwater in the subsurface are intimately connected and exchange water many times along the way (adapted from NASA, 2020).[\/caption]\r\n\r\nThe mechanisms of these exchanges involve water transfer from the atmosphere to the surface and subsurface, and back from the subsurface to the surface and the atmosphere; through precipitation, infiltration, evapotranspiration, and precipitation recycling, as well as through gaining and losing streams. These three transport systems periodically \u201cswitch roles\u201d with respect to which one is transporting a particular drop of water from where it first falls on the continent to where it arrives in the ocean. <strong>These interactions \u201cpower\u201d the global water flow system.<\/strong>","rendered":"<p>Zooming farther out provides an even larger view of the groundwater portion of the hydrologic cycle, extending from the continental divide to the coastal ocean (Figure\u00a035). Broadly, there are two end members of the continental scale system:<\/p>\n<ul>\n<li>the headwaters in mountainous regions near the continental divide; and,<\/li>\n<li>the lower basins in flat regions near the coast.<\/li>\n<\/ul>\n<p>Connecting the headwaters and the lower basins are two, large, continental\u2011scale, terrestrial, water transport systems: one above ground and the other in the subsurface.<\/p>\n<ul>\n<li>The above ground system is the readily observable stream network, which is concentrated (in channels) and is largely two\u2011dimensional (hugging the land surface). Small upland streams cascade over the surface and converge down\u2011gradient in an orderly manner.<\/li>\n<li>The subsurface system is the difficult\u2011to\u2011observe groundwater system, which is diffuse (not in channels nor tunnels, except in karst terrain, but rather in pores and fractures of geologic materials), which, relative to the stream network, is three\u2011dimensional (with flow paths that do not necessarily follow the shape of the land surface). Patterns of groundwater flow are less orderly than the stream network because groundwater is driven by multi\u2011scale hydraulic head gradients that are strongly deflected or contorted by complex geologic structures.<a id=\"Figure35\"><\/a><\/li>\n<\/ul>\n<figure id=\"attachment_202\" aria-describedby=\"caption-attachment-202\" style=\"width: 1024px\" class=\"wp-caption alignnone\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-202 size-large\" src=\"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig35-1024x793.jpg\" alt=\"Figure showing groundwater flow at the continental scale\" width=\"1024\" height=\"793\" srcset=\"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig35-1024x793.jpg 1024w, https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig35-300x232.jpg 300w, https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig35-768x595.jpg 768w, https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig35-65x50.jpg 65w, https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig35-225x174.jpg 225w, https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig35-350x271.jpg 350w, https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig35.jpg 1070w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><figcaption id=\"caption-attachment-202\" class=\"wp-caption-text\"><strong>Figure 35 &#8211;<\/strong> The continental view, showing the spatial context of: a) both losing and gaining streams as well as submarine groundwater discharge; and, b) the multi scale nature of groundwater flow systems with shallow, local flow systems nested within deeper intermediate systems which are nested in regional flow systems. This illustrates the long distance hydrologic connectivity of the surface and subsurface water system through exchange between rivers and groundwater, and discharge of rivers and groundwater to the ocean (adapted from Winter et al. 1998).<\/figcaption><\/figure>\n<p>Water is exchanged between the surface and subsurface as illustrated by gaining and losing streams and submarine seeps (Figure\u00a035a), and local and regional groundwater flow systems develope (Figure\u00a035b). The <em>local systems tend to be shallow and short<\/em>, and respond to short\u2011term rain events and seasonal changes in climatic conditions. The <em>regional systems are deeper and longer<\/em>. Regional systems tend to \u201crecord\u201d the climate conditions from decades to centuries to millenia ago. For example, a gaining stream in the lower reaches of a basin that is supplied by regional groundwater flow may never run dry, even after long droughts because the groundwater was recharged thousands or tens of thousands years ago when the climate was different.<\/p>\n<p>As shown in the large\u2011scale continental view of Figure\u00a035, groundwater can directly discharge into the ocean along the coast of the continent. This is referred to as <em>submarine groundwater discharge<\/em>. Such features were understood and utilized by sea\u2011faring people to locate fresh water long ago as illustrated in Figure\u00a036. Much submarine groundwater discharge occurs close to shore such as in bays and estuaries.<\/p>\n<figure id=\"attachment_205\" aria-describedby=\"caption-attachment-205\" style=\"width: 864px\" class=\"wp-caption alignnone\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-205 size-full\" src=\"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig36.jpg\" alt=\"Figure illustrating the use of submarine springs for drinking water by seafarers\" width=\"864\" height=\"572\" srcset=\"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig36.jpg 864w, https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig36-300x199.jpg 300w, https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig36-768x508.jpg 768w, https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig36-65x43.jpg 65w, https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig36-225x149.jpg 225w, https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig36-350x232.jpg 350w\" sizes=\"auto, (max-width: 864px) 100vw, 864px\" \/><figcaption id=\"caption-attachment-205\" class=\"wp-caption-text\"><strong>Figure 36 &#8211;<\/strong> Submarine springs were correctly understood and utilized for drinking water by seafaring people long ago: a) salt water; b) fresh water; c) low permeability geologic layers; and d) permeable geologic layer. (after Humboldt (1825) who drew the submarine spring diagram as published in the translation by Thrasher in 1856).<\/figcaption><\/figure>\n<p>In summary, there are <strong>three continental\u2011scale water transport systems<\/strong>:<\/p>\n<ol>\n<li>The <strong>atmosphere<\/strong><strong>;<\/strong><\/li>\n<li>The <strong>stream networks<\/strong><strong>;<\/strong> and,<\/li>\n<li>The <strong>groundwater systems<\/strong><strong>. <\/strong><\/li>\n<\/ol>\n<p>These continental\u2011scale systems are not isolated. They do not simply deliver continental rainfall back to the ocean in parallel flow systems, rather they are intimately connected and exchange water many times along the way (Figure\u00a037).<\/p>\n<figure id=\"attachment_207\" aria-describedby=\"caption-attachment-207\" style=\"width: 1024px\" class=\"wp-caption alignnone\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-207 size-large\" src=\"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig37-1024x566.jpg\" alt=\"Figure showing three continental scale water transport systems\" width=\"1024\" height=\"566\" srcset=\"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig37-1024x566.jpg 1024w, https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig37-300x166.jpg 300w, https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig37-768x425.jpg 768w, https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig37-1536x849.jpg 1536w, https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig37-65x36.jpg 65w, https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig37-225x124.jpg 225w, https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig37-350x194.jpg 350w, https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-content\/uploads\/sites\/2\/2020\/09\/Fig37.jpg 1570w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><figcaption id=\"caption-attachment-207\" class=\"wp-caption-text\"><strong>Figure 37 &#8211;<\/strong> Three continental scale water transport systems: air circulation in the atmosphere, stream networks on surface, and groundwater in the subsurface are intimately connected and exchange water many times along the way (adapted from NASA, 2020).<\/figcaption><\/figure>\n<p>The mechanisms of these exchanges involve water transfer from the atmosphere to the surface and subsurface, and back from the subsurface to the surface and the atmosphere; through precipitation, infiltration, evapotranspiration, and precipitation recycling, as well as through gaining and losing streams. These three transport systems periodically \u201cswitch roles\u201d with respect to which one is transporting a particular drop of water from where it first falls on the continent to where it arrives in the ocean. <strong>These interactions \u201cpower\u201d the global water flow system.<\/strong><\/p>\n","protected":false},"author":1,"menu_order":10,"template":"","meta":{"pb_show_title":"on","pb_short_title":"","pb_subtitle":"","pb_authors":[],"pb_section_license":""},"chapter-type":[],"contributor":[],"license":[],"class_list":["post-107","chapter","type-chapter","status-publish","hentry"],"part":75,"_links":{"self":[{"href":"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-json\/pressbooks\/v2\/chapters\/107","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-json\/pressbooks\/v2\/chapters"}],"about":[{"href":"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-json\/wp\/v2\/types\/chapter"}],"author":[{"embeddable":true,"href":"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-json\/wp\/v2\/users\/1"}],"version-history":[{"count":0,"href":"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-json\/pressbooks\/v2\/chapters\/107\/revisions"}],"part":[{"href":"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-json\/pressbooks\/v2\/parts\/75"}],"metadata":[{"href":"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-json\/pressbooks\/v2\/chapters\/107\/metadata\/"}],"wp:attachment":[{"href":"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-json\/wp\/v2\/media?parent=107"}],"wp:term":[{"taxonomy":"chapter-type","embeddable":true,"href":"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-json\/pressbooks\/v2\/chapter-type?post=107"},{"taxonomy":"contributor","embeddable":true,"href":"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-json\/wp\/v2\/contributor?post=107"},{"taxonomy":"license","embeddable":true,"href":"https:\/\/books.gw-project.org\/groundwater-in-our-water-cycle\/wp-json\/wp\/v2\/license?post=107"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}