Standard

Principles used in compiling and editing relief features of soviet bathymetric maps as applied to the western indian ocean. / Petrova, Tatiyana M.; Aliyev, Takhir A.; Scepan, Joseph.

в: Marine Geodesy, Том 14, № 2, 01.01.1990, стр. 143-149.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

Harvard

APA

Vancouver

Author

Petrova, Tatiyana M. ; Aliyev, Takhir A. ; Scepan, Joseph. / Principles used in compiling and editing relief features of soviet bathymetric maps as applied to the western indian ocean. в: Marine Geodesy. 1990 ; Том 14, № 2. стр. 143-149.

BibTeX

@article{7e60efaaca2a4db8b5dac16c369886fa,
title = "Principles used in compiling and editing relief features of soviet bathymetric maps as applied to the western indian ocean",
abstract = "Some principles used in compiling and editing Soviet bathymetric charts are presented. We particularly focus on mapping relief of the ocean floor. We consider various morphologic and morphometric features of the ocean floor and describe how these features are represented on bathymetric maps. Morphologic features are those that are identified from source data but cannot be measured on the original map. Morphometric features are those for which quantitative data (i.e., absolute and relative height, slope gradient, extent) can be derived from source maps. For this analysis, we examine the Western Indian Ocean, and five major ocean-bottom relief features are identified and described for this area: The continental shelf, the continental slope, hollows, local ridges, and midocean ridges. The choice of bathymetric contour interval (h) is the most important factor in accurate editing of ocean floor relief and we describe nine important physical parameters that must be evaluated for identifying proper contour interval. We also describe the methodology for determining optimum mapping scale and the bathymetric scale range. A four-step process for accurate map editing is outlined. This method can be used to edit features of single maps as well as to evaluate the accuracy and visual interpretability between maps.",
author = "Petrova, {Tatiyana M.} and Aliyev, {Takhir A.} and Joseph Scepan",
year = "1990",
month = jan,
day = "1",
doi = "10.1080/15210609009379652",
language = "English",
volume = "14",
pages = "143--149",
journal = "Marine Geodesy",
issn = "0149-0419",
publisher = "Taylor & Francis",
number = "2",

}

RIS

TY - JOUR

T1 - Principles used in compiling and editing relief features of soviet bathymetric maps as applied to the western indian ocean

AU - Petrova, Tatiyana M.

AU - Aliyev, Takhir A.

AU - Scepan, Joseph

PY - 1990/1/1

Y1 - 1990/1/1

N2 - Some principles used in compiling and editing Soviet bathymetric charts are presented. We particularly focus on mapping relief of the ocean floor. We consider various morphologic and morphometric features of the ocean floor and describe how these features are represented on bathymetric maps. Morphologic features are those that are identified from source data but cannot be measured on the original map. Morphometric features are those for which quantitative data (i.e., absolute and relative height, slope gradient, extent) can be derived from source maps. For this analysis, we examine the Western Indian Ocean, and five major ocean-bottom relief features are identified and described for this area: The continental shelf, the continental slope, hollows, local ridges, and midocean ridges. The choice of bathymetric contour interval (h) is the most important factor in accurate editing of ocean floor relief and we describe nine important physical parameters that must be evaluated for identifying proper contour interval. We also describe the methodology for determining optimum mapping scale and the bathymetric scale range. A four-step process for accurate map editing is outlined. This method can be used to edit features of single maps as well as to evaluate the accuracy and visual interpretability between maps.

AB - Some principles used in compiling and editing Soviet bathymetric charts are presented. We particularly focus on mapping relief of the ocean floor. We consider various morphologic and morphometric features of the ocean floor and describe how these features are represented on bathymetric maps. Morphologic features are those that are identified from source data but cannot be measured on the original map. Morphometric features are those for which quantitative data (i.e., absolute and relative height, slope gradient, extent) can be derived from source maps. For this analysis, we examine the Western Indian Ocean, and five major ocean-bottom relief features are identified and described for this area: The continental shelf, the continental slope, hollows, local ridges, and midocean ridges. The choice of bathymetric contour interval (h) is the most important factor in accurate editing of ocean floor relief and we describe nine important physical parameters that must be evaluated for identifying proper contour interval. We also describe the methodology for determining optimum mapping scale and the bathymetric scale range. A four-step process for accurate map editing is outlined. This method can be used to edit features of single maps as well as to evaluate the accuracy and visual interpretability between maps.

UR - http://www.scopus.com/inward/record.url?scp=0025524893&partnerID=8YFLogxK

U2 - 10.1080/15210609009379652

DO - 10.1080/15210609009379652

M3 - Article

AN - SCOPUS:0025524893

VL - 14

SP - 143

EP - 149

JO - Marine Geodesy

JF - Marine Geodesy

SN - 0149-0419

IS - 2

ER -

ID: 28292508