Javascript must be enabled to continue!
Distribution Trend of the Bottom Water at the Bay Mouth of Jiaozhou Bay
View through CrossRef
Based on the survey data of Jiaozhou Bay in May, June, July, August, September and October of 1980, the bottom water temperature and its horizontal distribution in Jiaozhou Bay were studied. The results showedthat the bottom water temperaturein Jiaozhou Bay rangedat a high level between 12.35℃to 25.72℃and a low level between 10.18℃to 24.58 ℃in May, June, July, August, September and October. From May to October, the bottom water temperature in Jiaozhou Bay was moderately high. In May, June, July and August, a high temperature zone formed around the waterinside the bay mouth, and the bottom water temperaturereached 12.35℃to 25.72℃.From May to August, the bottom water temperaturefirst increased in the watersinside the bay mouth, followed by the water at the bay mouth, withthe water outside the bay mouthas the end. In September and October, the temperature of the eastern coastal water outside Jiaozhou Bay ranged from 20.00℃to 24.43℃, and a high temperature zone formed around there. From September to October,the bottom water temperaturefirst decreased in the water inside the bay mouth, followed by the water at the bay mouth, with the water outside the bay mouthas the end. According to Yang Dongfang's definition of “Cryogenic Low Water Mass”, a cryogenic water mass formed in the bottom water at the bay mouthin September and extended widely among the water inside the bay mouth-at the bay mouth-in the southern part outside the bay mouthwith a temperature of 23.79℃to 23.91℃.
Title: Distribution Trend of the Bottom Water at the Bay Mouth of Jiaozhou Bay
Description:
Based on the survey data of Jiaozhou Bay in May, June, July, August, September and October of 1980, the bottom water temperature and its horizontal distribution in Jiaozhou Bay were studied.
The results showedthat the bottom water temperaturein Jiaozhou Bay rangedat a high level between 12.
35℃to 25.
72℃and a low level between 10.
18℃to 24.
58 ℃in May, June, July, August, September and October.
From May to October, the bottom water temperature in Jiaozhou Bay was moderately high.
In May, June, July and August, a high temperature zone formed around the waterinside the bay mouth, and the bottom water temperaturereached 12.
35℃to 25.
72℃.
From May to August, the bottom water temperaturefirst increased in the watersinside the bay mouth, followed by the water at the bay mouth, withthe water outside the bay mouthas the end.
In September and October, the temperature of the eastern coastal water outside Jiaozhou Bay ranged from 20.
00℃to 24.
43℃, and a high temperature zone formed around there.
From September to October,the bottom water temperaturefirst decreased in the water inside the bay mouth, followed by the water at the bay mouth, with the water outside the bay mouthas the end.
According to Yang Dongfang's definition of “Cryogenic Low Water Mass”, a cryogenic water mass formed in the bottom water at the bay mouthin September and extended widely among the water inside the bay mouth-at the bay mouth-in the southern part outside the bay mouthwith a temperature of 23.
79℃to 23.
91℃.
Related Results
Use of Formation Water and Associated Gases and their Simultaneous Utilization for Obtaining Microelement Concentrates Fresh Water and Drinking Water
Use of Formation Water and Associated Gases and their Simultaneous Utilization for Obtaining Microelement Concentrates Fresh Water and Drinking Water
Abstract Purpose: The invention relates to the oil industry, inorganic chemistry, in particular, to the methods of complex processing of formation water, using flare gas of oil and...
Diets and Seasonal Ingestion Rates of Aurelia coerulea (Cnidaria: Scyphozoa) Polyps by in situ Feeding Experiments in Jiaozhou Bay, China
Diets and Seasonal Ingestion Rates of Aurelia coerulea (Cnidaria: Scyphozoa) Polyps by in situ Feeding Experiments in Jiaozhou Bay, China
The benthic scyphopolyp population is an important stage in the scyphozoan lifecycle. Nevertheless, few studies have detailed the natural feeding and quantified the energy flux of ...
Substitusi Tepung Ampas Tahu Pada Pengolahan Kue Bay Tat
Substitusi Tepung Ampas Tahu Pada Pengolahan Kue Bay Tat
Tofu dregs flour is obtained from drying tofu dregs, which still have high protein and fiber content. It can be used as a substitute for wheat flour in processing a typical Bengkul...
Mapping regional oral dryness
Mapping regional oral dryness
The Regional Oral Dryness Inventory (RODI), a newly developed questionnaire which quantifies the severity of dryness at various locations in the mouth. It was found that there is a...
Climate change modeling for water resources management : Tana Sub-Basin, Ethiopia
Climate change modeling for water resources management : Tana Sub-Basin, Ethiopia
This study, conducted in the Tana Sub-basin, Ethiopia, aimed to model the impact of climate
change on water resources management. The Soil and Water Assessment Tool (SWAT), SPI
gen...
Evaluation of Water Balance and Water Use Efficiency with the Development of Water-Saving Irrigation in the Yanqi Basin Irrigation District of China
Evaluation of Water Balance and Water Use Efficiency with the Development of Water-Saving Irrigation in the Yanqi Basin Irrigation District of China
Irrigation water is the main type of water consumption in the Yanqi Basin irrigation district of Xinjiang, which is an oasis-type irrigation district in the arid region of Northwes...
Salinity Structure Within The Estuary Of Bintuni Bay, At The Southern Part Of Bird Head Of West Papua, Indonesia
Salinity Structure Within The Estuary Of Bintuni Bay, At The Southern Part Of Bird Head Of West Papua, Indonesia
Bintuni Bay is a semi-closed bay which a lot of big rivers flow into the bay and bring a huge amount of freshwater. This bay is not directly connected to the open sea but separated...

