Subsurface temperature maximum in a stratified estuary
A subsurface temperature maximum recorded in the highly stratified Krka Estuary is described. The maximum is located on the lower edge of a steep halocline and reaches the highest temperature in the Adriatic Sea. Temperatures of up to 31 °C were recorded. The development of the maximum and its persi...
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Veröffentlicht in: | Marine chemistry 1991, Vol.32 (2), p.163-170 |
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container_title | Marine chemistry |
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creator | Legovic, T Grzetic, Z Zutic, V |
description | A subsurface temperature maximum recorded in the highly stratified Krka Estuary is described. The maximum is located on the lower edge of a steep halocline and reaches the highest temperature in the Adriatic Sea. Temperatures of up to 31 °C were recorded. The development of the maximum and its persistence during summer is the consequence of a relatively thin and transparent brackish water layer while the entrainment of the seawater is weak. The maximum may be recorded from the middle of April until the end of October. |
doi_str_mv | 10.1016/0304-4203(91)90035-U |
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The maximum is located on the lower edge of a steep halocline and reaches the highest temperature in the Adriatic Sea. Temperatures of up to 31 °C were recorded. The development of the maximum and its persistence during summer is the consequence of a relatively thin and transparent brackish water layer while the entrainment of the seawater is weak. 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The maximum is located on the lower edge of a steep halocline and reaches the highest temperature in the Adriatic Sea. Temperatures of up to 31 °C were recorded. The development of the maximum and its persistence during summer is the consequence of a relatively thin and transparent brackish water layer while the entrainment of the seawater is weak. 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The maximum is located on the lower edge of a steep halocline and reaches the highest temperature in the Adriatic Sea. Temperatures of up to 31 °C were recorded. The development of the maximum and its persistence during summer is the consequence of a relatively thin and transparent brackish water layer while the entrainment of the seawater is weak. The maximum may be recorded from the middle of April until the end of October.</abstract><pub>Elsevier B.V</pub><doi>10.1016/0304-4203(91)90035-U</doi><tpages>8</tpages></addata></record> |
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subjects | Brackish Marine |
title | Subsurface temperature maximum in a stratified estuary |
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