Access the full text.
Sign up today, get DeepDyve free for 14 days.
V. I. Zaburdaev (1999)
Systems of Monitoring of the Environment [in Russian]
P. Saunders (1981)
Practical Conversion of Pressure to DepthJournal of Physical Oceanography, 11
K. Kremling (1974)
Relation Between Chlorinity and Conductivity Salinity in Black Sea Water. The Black Sea-Geology, Chemistry and Biology
F. Millero, P. Chetirkin (1980)
The density of Caspian Sea waters, 27
L. I. Ivanov, I. Y. Shkvorets (1995)
Thermohaline structure of abyssal and bottom waters in the Black SeaMorsk. Gidrofiz. Zh., 6
N. Fofonoff, R. Millard (1983)
Algorithms for Computation of Fundamental Properties of Seawater. Endorsed by Unesco/SCOR/ICES/IAPSO Joint Panel on Oceanographic Tables and Standards and SCOR Working Group 51. Unesco Technical Papers in Marine Science, No. 44.
J. Murray, Z. Top, E. Özsoy (1991)
Hydrographic properties and ventilation of the Black Sea, 38
N. P. Fofonoff, R. C. Millard (1983)
Algorithms for computation of fundamental properties of seawaterUNESCO Tech. Pap. Mar. Sci., 44
P. Saunders, N. Fofonoff (1976)
Conversion of pressure to depth in the oceanDeep Sea Research and Oceanographic Abstracts, 23
T. Oguz, S. Besiktepe, O. Basturk (1993)
CoMSBlack 92: Report of the Physical and Chemical Intercalibration Workshop, CoMSBlack 93-102 Tech. Rep. (May 1993)
On the basis of the generalization of the concept of “standard” ocean to the Black Sea, we deduce practical formulas for the conversion of pressure into depth and vice versa depending on the latitude of the place with regard for the equation of state for 1980. The error of these relations for the “standard” Black Sea (whose salinity is equal to 22.2 at a temperature of +9°C from the surface to the bottom) does not exceed ±0.2 m and ±0.2 dbar. The difference between the “practical” and actual depths in winter and summer periods does not exceed ±0.35 m for depths varying within range 0–2000 m. The proposed practical formulas enable one to simplify the procedure of rapid evaluation of depth (or pressure) in real time by excluding the procedure of integration over a specific volume.
Physical Oceanography – Springer Journals
Published: Oct 21, 2004
Read and print from thousands of top scholarly journals.
Already have an account? Log in
Bookmark this article. You can see your Bookmarks on your DeepDyve Library.
To save an article, log in first, or sign up for a DeepDyve account if you don’t already have one.
Copy and paste the desired citation format or use the link below to download a file formatted for EndNote
Access the full text.
Sign up today, get DeepDyve free for 14 days.
All DeepDyve websites use cookies to improve your online experience. They were placed on your computer when you launched this website. You can change your cookie settings through your browser.