{"id":217,"date":"2017-01-23T16:35:54","date_gmt":"2017-01-23T16:35:54","guid":{"rendered":"https:\/\/pressbooks.ccconline.org\/introduction-to-oceanography\/chapter\/6-2-temperature\/"},"modified":"2021-10-26T20:51:16","modified_gmt":"2021-10-26T20:51:16","slug":"6-2-temperature","status":"publish","type":"chapter","link":"https:\/\/pressbooks.ccconline.org\/introduction-to-oceanography\/chapter\/6-2-temperature\/","title":{"raw":"6.2 Temperature","rendered":"6.2 Temperature"},"content":{"raw":"Generally ocean temperatures range from about -2o<\/sup> to 30o<\/sup> C (28-86o<\/sup> F). The warmest water tends to be surface water in low [pb_glossary id=\"894\"]latitude [\/pb_glossary] regions, while the surface water at the poles is obviously much colder (Figure 6.2.1). Note that at equivalent latitudes, water on the eastern side of the ocean basins is colder than the water on the western side. This has to do with the pattern of surface currents, as described in section 9.1<\/a>. Even though surface water can be quite warm, most of the water in the oceans is deeper, colder water, so that the average temperature of the entire ocean is about 4o<\/sup> C, which is roughly the temperature inside your refrigerator.\r\n\r\n \r\n\r\n[caption id=\"attachment_212\" align=\"aligncenter\" width=\"1007\"]\"Global<\/a> Figure 6.2.1<\/strong> Global average annual sea surface temperature (Stephen Earle, \"Physical Geology\").[\/caption]\r\n\r\nA typical temperature profile for open ocean, mid-latitude water is shown in Figure 6.2.2. Water is warmest at the surface, as it is warmed by the sun, and the sun's rays can only penetrate depths less than 1000 m (section 6.5<\/a>). Since the surface water is warmer it is also less dense than the deep water (section 6.3<\/a>), so it remains at the surface where it can be warmed even more. Temperature is fairly constant in the upper 100-200 m in what is called the [pb_glossary id=\"950\"]mixed layer[\/pb_glossary]<\/strong>. The mixed layer results from surface winds, waves, and currents that mix the upper water and distribute the heat throughout this layer. Below the mixed layer there is a rapid decline in temperature over a fairly narrow increase in depth. This is called the [pb_glossary id=\"1222\"]thermocline[\/pb_glossary]<\/strong>. Below the thermocline the deep ocean temperature is fairly constant at about 2o<\/sup> C, continuing down to the bottom. There is little temperature change in the deep ocean, as it is far removed from significant heat sources, making it one of the most thermally stable regions on earth. Temperature may fluctuate by less than half a degree per year in the deep ocean (Figure 6.2.3).\r\n\r\n[caption id=\"attachment_213\" align=\"aligncenter\" width=\"773\"]\"Typical<\/a> Figure 6.2.2<\/strong> Typical open ocean temperature profile for a mid-latitude region, showing the mixed layer, steep thermocline, and relatively stable temperature at depth (Public domain via Wikimedia Commons).[\/caption]\r\n\r\n[caption id=\"attachment_214\" align=\"aligncenter\" width=\"1024\"]\"Temperature<\/a> Figure 6.2.3<\/strong> Temperature profile across the Atlantic Ocean from the coast of Florida to the coast of Africa (inset). There is rapid temperature change near the surface in the thermocline zone, but the deep water temperature is fairly stable (eWOCE, http:\/\/www.ewoce.org\/gallery\/eWOCE_Tables.html#Atlantic).[\/caption]\r\n\r\nTemperature profiles vary at different latitudes, as the surface water is warmer near the equator and colder at the poles. In low latitude tropical regions the sea surface is much warmer, leading to a highly pronounced [pb_glossary id=\"1222\"]thermocline [\/pb_glossary] (Figure 6.2.4). Additionally, there is not much seasonal change in surface temperature in tropical regions, so there is little seasonal change in the profiles. In high latitude (polar) regions, there is little difference between the surface temperature and the deep water temperature, and temperature is fairly constant (and cold) at all depths. Polar waters therefore lack a strong thermocline, and as with tropical water, there is little seasonal change in temperatures. Mid-latitude temperate regions show greater seasonal fluctuations in surface temperature than the poles or the tropics; an 8-15o<\/sup> C difference from summer to winter in temperate zones, compared to only ~2o<\/sup> C in polar and tropical areas. In temperate regions, the surface water is much warmer in the summer and the thermocline is more pronounced compared to the winter months. But in the winter the thermocline is deeper<\/em> at mid-latitudes than it is in the summer. This is because winter storms churn up the surface water more than occurs in the summer, creating a deeper [pb_glossary id=\"950\"]mixed layer[\/pb_glossary] and thus a deeper thermocline (Figure 6.2.5).\r\n\r\n[caption id=\"attachment_215\" align=\"aligncenter\" width=\"545\"]\"Representative<\/a> Figure 6.2.4<\/strong> Representative temperature profiles for tropical, mid-latitude, and polar regions (PW).[\/caption]\r\n\r\n[caption id=\"attachment_216\" align=\"aligncenter\" width=\"539\"]\"In<\/a> Figure 6.2.5<\/strong> In temperate regions, the mixed layer is deeper and the thermocline less pronounced in the winter compared to the summer (PW).[\/caption]\r\n\r\nDue to the high heat capacity of water, daily fluctuations in ocean temperature are fairly insignificant.","rendered":"

Generally ocean temperatures range from about -2o<\/sup> to 30o<\/sup> C (28-86o<\/sup> F). The warmest water tends to be surface water in low latitude <\/a> regions, while the surface water at the poles is obviously much colder (Figure 6.2.1). Note that at equivalent latitudes, water on the eastern side of the ocean basins is colder than the water on the western side. This has to do with the pattern of surface currents, as described in section 9.1<\/a>. Even though surface water can be quite warm, most of the water in the oceans is deeper, colder water, so that the average temperature of the entire ocean is about 4o<\/sup> C, which is roughly the temperature inside your refrigerator.<\/p>\n

 <\/p>\n

\"Global<\/a>
Figure 6.2.1<\/strong> Global average annual sea surface temperature (Stephen Earle, “Physical Geology”).<\/figcaption><\/figure>\n

A typical temperature profile for open ocean, mid-latitude water is shown in Figure 6.2.2. Water is warmest at the surface, as it is warmed by the sun, and the sun’s rays can only penetrate depths less than 1000 m (section 6.5<\/a>). Since the surface water is warmer it is also less dense than the deep water (section 6.3<\/a>), so it remains at the surface where it can be warmed even more. Temperature is fairly constant in the upper 100-200 m in what is called the mixed layer<\/a><\/strong>. The mixed layer results from surface winds, waves, and currents that mix the upper water and distribute the heat throughout this layer. Below the mixed layer there is a rapid decline in temperature over a fairly narrow increase in depth. This is called the thermocline<\/a><\/strong>. Below the thermocline the deep ocean temperature is fairly constant at about 2o<\/sup> C, continuing down to the bottom. There is little temperature change in the deep ocean, as it is far removed from significant heat sources, making it one of the most thermally stable regions on earth. Temperature may fluctuate by less than half a degree per year in the deep ocean (Figure 6.2.3).<\/p>\n

\"Typical<\/a>
Figure 6.2.2<\/strong> Typical open ocean temperature profile for a mid-latitude region, showing the mixed layer, steep thermocline, and relatively stable temperature at depth (Public domain via Wikimedia Commons).<\/figcaption><\/figure>\n
\"Temperature<\/a>
Figure 6.2.3<\/strong> Temperature profile across the Atlantic Ocean from the coast of Florida to the coast of Africa (inset). There is rapid temperature change near the surface in the thermocline zone, but the deep water temperature is fairly stable (eWOCE, http:\/\/www.ewoce.org\/gallery\/eWOCE_Tables.html#Atlantic).<\/figcaption><\/figure>\n

Temperature profiles vary at different latitudes, as the surface water is warmer near the equator and colder at the poles. In low latitude tropical regions the sea surface is much warmer, leading to a highly pronounced thermocline <\/a> (Figure 6.2.4). Additionally, there is not much seasonal change in surface temperature in tropical regions, so there is little seasonal change in the profiles. In high latitude (polar) regions, there is little difference between the surface temperature and the deep water temperature, and temperature is fairly constant (and cold) at all depths. Polar waters therefore lack a strong thermocline, and as with tropical water, there is little seasonal change in temperatures. Mid-latitude temperate regions show greater seasonal fluctuations in surface temperature than the poles or the tropics; an 8-15o<\/sup> C difference from summer to winter in temperate zones, compared to only ~2o<\/sup> C in polar and tropical areas. In temperate regions, the surface water is much warmer in the summer and the thermocline is more pronounced compared to the winter months. But in the winter the thermocline is deeper<\/em> at mid-latitudes than it is in the summer. This is because winter storms churn up the surface water more than occurs in the summer, creating a deeper mixed layer<\/a> and thus a deeper thermocline (Figure 6.2.5).<\/p>\n

\"Representative<\/a>
Figure 6.2.4<\/strong> Representative temperature profiles for tropical, mid-latitude, and polar regions (PW).<\/figcaption><\/figure>\n
\"In<\/a>
Figure 6.2.5<\/strong> In temperate regions, the mixed layer is deeper and the thermocline less pronounced in the winter compared to the summer (PW).<\/figcaption><\/figure>\n

Due to the high heat capacity of water, daily fluctuations in ocean temperature are fairly insignificant.<\/p>\n

definition<\/span>