Abstract
The results of hydrophysical studies in Red Sea hot brines prefaced with historical information are presented. The CTD-recorder readings show stratification of the upper brine in the Atlantis II Deep into meter-scale layers, in agreement with laboratory findings. Repeated soundings with the AIST CTD meter of the upper brine interface in the Valdivia Deep recorded internal waves of 3 to 4-h periods. The observations show the different nature of brines in the four deeps studied and the lack of contact between the brine layers of the Chain and Discovery deeps.
Citation Formats
Monin, A S, and Plakhin, E A.
Stratification and space-time variability of Red Sea hot brines.
United Kingdom: N. p.,
1982.
Web.
doi:10.1016/0198-0149(82)90008-5.
Monin, A S, & Plakhin, E A.
Stratification and space-time variability of Red Sea hot brines.
United Kingdom.
https://doi.org/10.1016/0198-0149(82)90008-5
Monin, A S, and Plakhin, E A.
1982.
"Stratification and space-time variability of Red Sea hot brines."
United Kingdom.
https://doi.org/10.1016/0198-0149(82)90008-5.
@misc{etde_5947007,
title = {Stratification and space-time variability of Red Sea hot brines}
author = {Monin, A S, and Plakhin, E A}
abstractNote = {The results of hydrophysical studies in Red Sea hot brines prefaced with historical information are presented. The CTD-recorder readings show stratification of the upper brine in the Atlantis II Deep into meter-scale layers, in agreement with laboratory findings. Repeated soundings with the AIST CTD meter of the upper brine interface in the Valdivia Deep recorded internal waves of 3 to 4-h periods. The observations show the different nature of brines in the four deeps studied and the lack of contact between the brine layers of the Chain and Discovery deeps.}
doi = {10.1016/0198-0149(82)90008-5}
journal = []
volume = {29:11A}
journal type = {AC}
place = {United Kingdom}
year = {1982}
month = {Nov}
}
title = {Stratification and space-time variability of Red Sea hot brines}
author = {Monin, A S, and Plakhin, E A}
abstractNote = {The results of hydrophysical studies in Red Sea hot brines prefaced with historical information are presented. The CTD-recorder readings show stratification of the upper brine in the Atlantis II Deep into meter-scale layers, in agreement with laboratory findings. Repeated soundings with the AIST CTD meter of the upper brine interface in the Valdivia Deep recorded internal waves of 3 to 4-h periods. The observations show the different nature of brines in the four deeps studied and the lack of contact between the brine layers of the Chain and Discovery deeps.}
doi = {10.1016/0198-0149(82)90008-5}
journal = []
volume = {29:11A}
journal type = {AC}
place = {United Kingdom}
year = {1982}
month = {Nov}
}