Scholarly record
HYDROLOGICAL CHARACTERISTICS OF SEVASTOPOL BAY
Abstract
Since 1998, MHI has been monitoring the hydrological and hydrochemical characteristics of the waters of the Sevastopol Bay. The purpose of this work is to study the hydrological characteristics of the waters of the Sevastopol Bay, according to the expedition research data of the MHI in 2006-2018. This paper uses data from 34 surveys from 2006?2018. Studies during the majority of surveys were carried out on a grid of 36 stations, with 3 stations being performed just before going to the bay, the rest in the Sevastopol bay itself. 11 expeditions were completed in the winter months, the spring - 8, in the summer - 2, in the autumn - 13. The measurements were carried out using a complex SHIK-01 with an oxygen channel and an automatic cassette of batometers and autonomous complexes GAP-12? and GAP-12A. During the observation period (from 2006 to 2018) there were significant fluctuations (up to 100C) of the bottom temperature associated with cold water inflow. In the area of Grafskaya Bay due to river flow r. Chernaya salinity varied within 14-17.5%0. In general, in the cold months the sea surface temperature dropped to 60C, in the summer months it warmed up to 26oC, the salinity of surface waters was 17.5-17.75%0
Publication Impact Profile
Publication details
References0
Structured references will appear here after the reference import pass. The count is preserved now so the scholarly record is not incomplete.
Citing literature
Number of times cited according to Crossref: 2
View or Download full articleAccess options
SWS access login
Login as SWS Scientific CommitteeLogin as SWS Scientific PartnerLogin as SWS AuthorAuthors and approved SWS contributors will read and export their own linked papers after identity matching by SWS profile, email and SGEM GlobalID.
For librarian assistance: [email protected]
Purchase Instant Access
- Article can be downloaded after successful payment.
- Article may be used according to SWS library access terms.
- Article cannot be redistributed.

