{"id":16,"date":"2020-08-17T06:00:00","date_gmt":"2020-08-17T06:00:00","guid":{"rendered":""},"modified":"2024-05-21T15:05:10","modified_gmt":"2024-05-21T15:05:10","slug":"concept-of-hydrologic-cycle-with-image-oceanography","status":"publish","type":"post","link":"https:\/\/abhijeetpandey.in\/edu\/physical-geography\/concept-of-hydrologic-cycle-with-image-oceanography\/16","title":{"rendered":"Concept of Hydrologic Cycle with Image: Oceanography"},"content":{"rendered":"<p><span style=\"font-family: arial; font-size: x-large;\">The hydrologic cycle is a conceptual model that describes the storage and movement of water between the biosphere, atmosphere, lithosphere, and the hydrosphere (see Figure 8b-1).&nbsp;<\/span><\/p>\n<p><span style=\"font-family: arial; font-size: x-large;\"><br \/><\/span><\/p>\n<p><span style=\"font-family: arial; font-size: x-large;\">Water on this planet can be stored in any one of the following reservoirs: atmosphere, oceans, lakes, rivers, soils, glaciers, snowfields, and groundwater.<\/span><\/p>\n<p><span style=\"font-family: arial; font-size: x-large;\"><br \/><\/span><\/p>\n<div style=\"clear: both; text-align: center;\"><a href=\"https:\/\/i0.wp.com\/blogger.googleusercontent.com\/img\/b\/R29vZ2xl\/AVvXsEjahxu4EsxLmbaiBj2y8WC7cMvs0ecflFVTyq1K1ssHnMJDehovuXdZQAAfJrQ69YCweqH6YqIUmkXRZz7ZWwsHBzXnkmwHSrvtaXKyJCHZVyApzQZ8-sTZEiHol7qMwY8i8G0TRifPI77z\/s924\/hydrocycle.gif?ssl=1\" style=\"margin-left: 1em; margin-right: 1em;\"><span style=\"font-family: arial; font-size: x-large;\"><img data-recalc-dims=\"1\" decoding=\"async\" border=\"0\" data-original-height=\"460\" data-original-width=\"924\" src=\"https:\/\/i0.wp.com\/abhijeetpandey.in\/edu\/wp-content\/uploads\/2020\/08\/hydrocycle.gif?w=640&#038;ssl=1\"  \/><\/span><\/a><\/div>\n<p><span style=\"font-family: arial; font-size: x-large;\"><br \/><\/span><\/p>\n<p style=\"text-align: center;\"><span style=\"font-family: arial; font-size: x-large;\">Figure 8b-1: Hydrologic Cycle.<\/span><\/p>\n<p><span style=\"font-family: arial; font-size: x-large;\"><br \/><\/span><\/p>\n<p><span style=\"font-family: arial; font-size: x-large;\">Water moves from one reservoir to another by way of processes like evaporation, condensation, precipitation, deposition, runoff, infiltration, sublimation, transpiration, melting, and groundwater flow.<\/span><\/p>\n<p><span style=\"font-family: arial; font-size: x-large;\"><br \/><\/span><\/p>\n<p><span style=\"font-family: arial; font-size: x-large;\">The oceans supply most of the evaporated water found in the atmosphere. Of this evaporated water, only 91% of it is returned to the ocean basins by way of precipitation. The remaining 9% is transported to areas over landmasses where climatological factors induce the formation of precipitation.&nbsp;<\/span><\/p>\n<p><span style=\"font-family: arial; font-size: x-large;\"><br \/><\/span><\/p>\n<p><span style=\"font-family: arial; font-size: x-large;\">The resulting imbalance between rates of evaporation and precipitation over land and ocean is corrected by runoff and groundwater flow to the oceans.<\/span><\/p>\n<p><span style=\"font-family: arial; font-size: x-large;\"><br \/><\/span><\/p>\n<p><span style=\"font-family: arial; font-size: x-large;\">The planetary water supply is dominated by the oceans (see Table 8b-1). Approximately 97% of all the water on the Earth is in the oceans. The other 3% is held as freshwater in glaciers and icecaps, groundwater, lakes, soil, the atmosphere, and within life.<\/span><\/p>\n<p><span style=\"font-family: arial; font-size: x-large;\"><br \/><\/span><\/p>\n<p style=\"text-align: center;\"><span style=\"font-family: arial; font-size: x-large;\">Table 8b-1: Inventory of water at the Earth&#8217;s surface<\/span><\/p>\n<p><center><\/p>\n<table border=\"1\" cellpadding=\"2\" cellspacing=\"0\">\n<tbody>\n<tr bgcolor=\"\">\n<td><span style=\"background-color: #cfe2f3; font-family: arial; font-size: x-large;\">Reservoir<\/span><\/td>\n<td>\n<div align=\"center\"><span style=\"background-color: #cfe2f3; font-family: arial; font-size: x-large;\">Volume<br \/>\n                                  (cubic km x 1,000,000) <\/span><\/div>\n<\/td>\n<td>\n<div align=\"center\"><span style=\"background-color: #cfe2f3; font-family: arial; font-size: x-large;\">Percent<br \/>\n                                  of Total <\/span><\/div>\n<\/td>\n<\/tr>\n<tr bgcolor=\"\">\n<td><span style=\"font-family: arial; font-size: x-large;\">Oceans<\/span><\/td>\n<td>\n<div align=\"center\"><span style=\"font-family: arial; font-size: x-large;\">1370 <\/span><\/div>\n<\/td>\n<td>\n<div align=\"center\"><span style=\"font-family: arial; font-size: x-large;\">97.25 <\/span><\/div>\n<\/td>\n<\/tr>\n<tr bgcolor=\"\">\n<td><span style=\"font-family: arial; font-size: x-large;\">Ice Caps and Glaciers<\/span><\/td>\n<td>\n<div align=\"center\"><span style=\"font-family: arial; font-size: x-large;\">29 <\/span><\/div>\n<\/td>\n<td>\n<div align=\"center\"><span style=\"font-family: arial; font-size: x-large;\">2.05 <\/span><\/div>\n<\/td>\n<\/tr>\n<tr bgcolor=\"\">\n<td><span style=\"font-family: arial; font-size: x-large;\">Groundwater <\/span><\/td>\n<td>\n<div align=\"center\"><span style=\"font-family: arial; font-size: x-large;\">9.5 <\/span><\/div>\n<\/td>\n<td>\n<div align=\"center\"><span style=\"font-family: arial; font-size: x-large;\">0.68 <\/span><\/div>\n<\/td>\n<\/tr>\n<tr bgcolor=\"\">\n<td><span style=\"font-family: arial; font-size: x-large;\">Lakes<\/span><\/td>\n<td>\n<div align=\"center\"><span style=\"font-family: arial; font-size: x-large;\">0.125 <\/span><\/div>\n<\/td>\n<td>\n<div align=\"center\"><span style=\"font-family: arial; font-size: x-large;\">0.01 <\/span><\/div>\n<\/td>\n<\/tr>\n<tr bgcolor=\"\">\n<td><span style=\"font-family: arial; font-size: x-large;\">Soil Moisture<\/span><\/td>\n<td>\n<div align=\"center\"><span style=\"font-family: arial; font-size: x-large;\">0.065<\/span><\/div>\n<\/td>\n<td>\n<div align=\"center\"><span style=\"font-family: arial; font-size: x-large;\">0.005 <\/span><\/div>\n<\/td>\n<\/tr>\n<tr bgcolor=\"\">\n<td><span style=\"font-family: arial; font-size: x-large;\">Atmosphere<\/span><\/td>\n<td>\n<div align=\"center\"><span style=\"font-family: arial; font-size: x-large;\">0.013 <\/span><\/div>\n<\/td>\n<td>\n<div align=\"center\"><span style=\"font-family: arial; font-size: x-large;\">0.001<\/span><\/div>\n<\/td>\n<\/tr>\n<tr bgcolor=\"\">\n<td><span style=\"font-family: arial; font-size: x-large;\">Streams and Rivers<\/span><\/td>\n<td>\n<div align=\"center\"><span style=\"font-family: arial; font-size: x-large;\">0.0017 <\/span><\/div>\n<\/td>\n<td>\n<div align=\"center\"><span style=\"font-family: arial; font-size: x-large;\">0.0001<\/span><\/div>\n<\/td>\n<\/tr>\n<tr bgcolor=\"\">\n<td>\n<div align=\"left\"><span style=\"font-family: arial; font-size: x-large;\">Biosphere<br \/>\n                                <\/span><\/div>\n<\/td>\n<td>\n<div align=\"center\"><span style=\"font-family: arial; font-size: x-large;\">0.0006 <\/span><\/div>\n<\/td>\n<td>\n<div align=\"center\"><span style=\"font-family: arial; font-size: x-large;\"> 0.00004<\/span><\/div>\n<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<p><\/center><span style=\"font-family: arial; font-size: x-large;\"><br \/><\/span><\/p>\n<div><span style=\"font-family: arial; font-size: x-large;\"><br \/><\/span><\/div>\n<div><span style=\"font-family: arial; font-size: x-large;\">Water is continually cycled between its various reservoirs. This cycling occurs through the processes of evaporation, condensation, precipitation, deposition, runoff, infiltration, sublimation, transpiration, melting, and groundwater flow.<\/span><\/div>\n<div><span style=\"font-family: arial; font-size: x-large;\"><br \/><\/span><\/div>\n<div><span style=\"font-family: arial; font-size: x-large;\"><br \/><\/span><\/div>\n<div><span style=\"font-family: arial; font-size: x-large;\">Table 8b-2 describes the ty[ical residence times of water in the major reservoirs. On average water is renewed in rivers once every 16 days. Water in the atmosphere is completely replaced once every 8 days.<\/span><\/div>\n<div><span style=\"font-family: arial; font-size: x-large;\"><br \/><\/span><\/div>\n<div><span style=\"font-family: arial; font-size: x-large;\"><br \/><\/span><\/div>\n<div><span style=\"font-family: arial; font-size: x-large;\">Slower rates of replacement occur in large lakes, glaciers, ocean bodies and groundwater. Replacement in these reservoirs can take from hundreds to thousands of years.&nbsp;<\/span><\/div>\n<div><span style=\"font-family: arial; font-size: x-large;\"><br \/><\/span><\/div>\n<div><span style=\"font-family: arial; font-size: x-large;\">Some of these resources (especially groundwater) are being used by humans at rates that far exceed their renewal times. This type of resource use is making this type of water effectively nonrenewable.<\/span><\/div>\n<div><span style=\"font-family: arial; font-size: x-large;\"><br \/><\/span><\/div>\n<div><span style=\"font-family: arial; font-size: x-large;\"><br \/><\/span><\/div>\n<div style=\"text-align: center;\"><span style=\"font-family: arial; font-size: x-large;\">Table 8b-2: Typical residence times of water found in various reserviors<\/span><\/div>\n<div><span style=\"font-family: arial; font-size: x-large;\"><br \/><\/span><\/div>\n<p><center><\/p>\n<table border=\"1\" cellpadding=\"2\" cellspacing=\"0\" style=\"height: 159px;\">\n<tbody>\n<tr bgcolor=\"\">\n<td height=\"19\" width=\"37%\">\n<p><span style=\"font-family: arial; font-size: x-large;\">&nbsp;<span style=\"background-color: #a2c4c9;\">Reservoir<\/span><\/span><\/p>\n<\/td>\n<td width=\"63%\">\n<p align=\"CENTER\"><span style=\"background-color: #a2c4c9; font-family: arial; font-size: x-large;\">Average Residence<br \/>\n                                Time <\/span><\/p>\n<\/td>\n<\/tr>\n<tr bgcolor=\"\">\n<td height=\"17\"><span style=\"font-family: arial; font-size: x-large;\">&nbsp;Glaciers<\/span><\/td>\n<td>\n<p align=\"CENTER\"><span style=\"font-family: arial; font-size: x-large;\">&nbsp;20 to 100<br \/>\n                                years <\/span><\/p>\n<\/td>\n<\/tr>\n<tr bgcolor=\"\">\n<td height=\"17\"><span style=\"font-family: arial; font-size: x-large;\">&nbsp;Seasonal<br \/>\n                                Snow Cover<\/span><\/td>\n<td>\n<p align=\"CENTER\"><span style=\"font-family: arial; font-size: x-large;\">&nbsp;2 to 6 months <\/span><\/p>\n<\/td>\n<\/tr>\n<tr bgcolor=\"\">\n<td height=\"17\"><span style=\"font-family: arial; font-size: x-large;\">&nbsp;Soil<br \/>\n                                Moisture<\/span><\/td>\n<td>\n<p align=\"CENTER\"><span style=\"font-family: arial; font-size: x-large;\">&nbsp;1 to 2 months <\/span><\/p>\n<\/td>\n<\/tr>\n<tr bgcolor=\"\">\n<td height=\"17\"><span style=\"font-family: arial; font-size: x-large;\">&nbsp;Groundwater:<br \/>\n                                Shallow<\/span><\/td>\n<td>\n<p align=\"CENTER\"><span style=\"font-family: arial; font-size: x-large;\">&nbsp;100 to 200<br \/>\n                                years <\/span><\/p>\n<\/td>\n<\/tr>\n<tr bgcolor=\"\">\n<td height=\"17\"><span style=\"font-family: arial; font-size: x-large;\">&nbsp;Groundwater:<br \/>\n                                Deep<\/span><\/td>\n<td>\n<p align=\"CENTER\"><span style=\"font-family: arial; font-size: x-large;\">&nbsp;10,000<br \/>\n                                years <\/span><\/p>\n<\/td>\n<\/tr>\n<tr bgcolor=\"\">\n<td height=\"17\"><span style=\"font-family: arial; font-size: x-large;\">&nbsp;Lakes<\/span><\/td>\n<td>\n<p align=\"CENTER\"><span style=\"font-family: arial; font-size: x-large;\">&nbsp;50 to 100<br \/>\n                                years <\/span><\/p>\n<\/td>\n<\/tr>\n<tr bgcolor=\"\">\n<td height=\"17\"><span style=\"font-family: arial; font-size: x-large;\">&nbsp;Rivers<\/span><\/td>\n<td>\n<p align=\"CENTER\"><span style=\"font-family: arial; font-size: x-large;\">&nbsp;2 to 6<br \/>\n                                months<\/span><\/p>\n<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<p><\/center><span style=\"font-family: arial; font-size: x-large;\"><br \/><\/span><\/p>\n<div>\n<p style=\"background: 0px 0px rgb(255, 255, 255); border: 0px; color: #5e5e5e; outline: 0px; padding: 0px; transition: all 0s ease 0s; vertical-align: baseline;\"><span style=\"background: 0px 0px; border: 0px; outline: 0px; padding: 0px; transition: all 0s ease 0s; vertical-align: baseline;\"><span style=\"font-family: arial; font-size: x-large;\">If you want to learn more Geography, please follow Geography Bees on&nbsp;<a href=\"https:\/\/fb.com\/geographybees\" rel=\"nofollow noopener\" style=\"background: 0px 0px; border: 0px; color: #ff4400; outline: 0px; padding: 0px; text-decoration-line: none; transition: all 0s ease 0s; vertical-align: baseline;\" target=\"_blank\">Facebook<\/a><\/span><\/span><\/p>\n<p style=\"background: 0px 0px rgb(255, 255, 255); border: 0px; color: #5e5e5e; outline: 0px; padding: 0px; transition: all 0s ease 0s; vertical-align: baseline;\"><span style=\"font-family: arial; font-size: x-large;\"><br style=\"outline: 0px; transition: all 0s ease 0s;\" \/><\/span><\/p>\n<p style=\"background: 0px 0px rgb(255, 255, 255); border: 0px; color: #5e5e5e; outline: 0px; padding: 0px; transition: all 0s ease 0s; vertical-align: baseline;\"><span style=\"background: 0px 0px; border: 0px; outline: 0px; padding: 0px; transition: all 0s ease 0s; vertical-align: baseline;\"><span style=\"font-family: arial; font-size: x-large;\">Happy Learning \ud83d\ude42<\/span><\/span><\/p>\n<\/div>\n","protected":false},"excerpt":{"rendered":"<p>The hydrologic cycle is a conceptual model that describes the storage and movement of water between the biosphere, atmosphere, lithosphere, and the hydrosphere (see Figure 8b-1).&nbsp; Water on this planet can be stored in any one of the following reservoirs: atmosphere, oceans, lakes, rivers, soils, glaciers, snowfields, and groundwater. Figure 8b-1: Hydrologic Cycle. Water moves [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":46,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"jetpack_post_was_ever_published":false,"_jetpack_newsletter_access":"","_jetpack_dont_email_post_to_subs":false,"_jetpack_newsletter_tier_id":0,"_jetpack_memberships_contains_paywalled_content":false,"_jetpack_memberships_contains_paid_content":false,"footnotes":""},"categories":[12,5],"tags":[],"class_list":["post-16","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-oceanography","category-physical-geography"],"jetpack_featured_media_url":"https:\/\/i0.wp.com\/abhijeetpandey.in\/edu\/wp-content\/uploads\/2020\/08\/hydrocycle.gif?fit=924%2C460&ssl=1","jetpack-related-posts":[],"jetpack_sharing_enabled":true,"_links":{"self":[{"href":"https:\/\/abhijeetpandey.in\/edu\/wp-json\/wp\/v2\/posts\/16","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/abhijeetpandey.in\/edu\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/abhijeetpandey.in\/edu\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/abhijeetpandey.in\/edu\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/abhijeetpandey.in\/edu\/wp-json\/wp\/v2\/comments?post=16"}],"version-history":[{"count":1,"href":"https:\/\/abhijeetpandey.in\/edu\/wp-json\/wp\/v2\/posts\/16\/revisions"}],"predecessor-version":[{"id":47,"href":"https:\/\/abhijeetpandey.in\/edu\/wp-json\/wp\/v2\/posts\/16\/revisions\/47"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/abhijeetpandey.in\/edu\/wp-json\/wp\/v2\/media\/46"}],"wp:attachment":[{"href":"https:\/\/abhijeetpandey.in\/edu\/wp-json\/wp\/v2\/media?parent=16"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/abhijeetpandey.in\/edu\/wp-json\/wp\/v2\/categories?post=16"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/abhijeetpandey.in\/edu\/wp-json\/wp\/v2\/tags?post=16"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}