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Massachusetts Institute of Technology

Edge analysis of seasonal variability in chlorophyll maps of the Black Sea

Abstract

dc:description.abstract

The use of remotely sensed oceanographic data would be greatly benefited by being able to detect circulation features automatically through edge detection. In the Black Sea, the use of edge detection to identify fronts can be used to study the effects of river input on circulation patterns and biological and physical interactions. The use of edge detection on remotely sensed chlorophyll data is limited by noisy data, inaccurate measurements, temporal and spatial gaps in data, and limitations on computational power. The algorithm described in this thesis utilizes image processing techniques to create an edge detection process that shows the effects of the Danube river input on Black Sea circulation patterns with little computational complexity.

Degree

thesis:*
Department dc:contributor.department
Massachusetts Institute of Technology. Dept. of Earth, Atmospheric, and Planetary Sciences.
Grantor dc:publisher
Massachusetts Institute of Technology
Year dc:date.issued
2000

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Deshpande, Ashwini G. (Ashwini Ganesh), 1977-
Advisor dc:contributor.advisor
  • Paola Malanotte-Rizzoli.

Subjects

dc:subject × 1

Rights

dc:rights
Statement dc:rights
  • M.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission.
Language dc:language.iso
eng

Identifiers

dc:identifier.*
Handle dc:identifier.uri
http://hdl.handle.net/1721.1/58165
OAI identifier oai:identifier
oai:dspace.mit.edu:1721.1/58165

Chain of custody

source
Harvested from
MIT
Base URL
dspace.mit.edu/oai/request
Last updated
2026-07-22
Source record
OAI-PMH GetRecord
citation

Deshpande, Ashwini G. (Ashwini Ganesh), 1977-. Edge analysis of seasonal variability in chlorophyll maps of the Black Sea. Massachusetts Institute of Technology, 2000. http://hdl.handle.net/1721.1/58165