Standard

Гипсографическая кривая подледно-подводной поверхности Земли. / Попов, Сергей Викторович.

In: ГЕОМОРФОЛОГИЯ, No. 4, 2015, p. 85-90.

Research output: Contribution to journal › Article › peer-review

Harvard

Попов, СВ 2015, 'Гипсографическая кривая подледно-подводной поверхности Земли', ГЕОМОРФОЛОГИЯ, no. 4, pp. 85-90. https://doi.org/10.15356/0435-4281-2015-4-85-90

APA

Попов, С. В. (2015). Гипсографическая кривая подледно-подводной поверхности Земли. ГЕОМОРФОЛОГИЯ, (4), 85-90. https://doi.org/10.15356/0435-4281-2015-4-85-90

Vancouver

Попов СВ. Гипсографическая кривая подледно-подводной поверхности Земли. ГЕОМОРФОЛОГИЯ. 2015;(4):85-90. https://doi.org/10.15356/0435-4281-2015-4-85-90

Author

Попов, Сергей Викторович. / Гипсографическая кривая подледно-подводной поверхности Земли. In: ГЕОМОРФОЛОГИЯ. 2015 ; No. 4. pp. 85-90.

BibTeX

@article{16c15bf35d0e4e4c8ae520baee9c17ba,
title = "Гипсографическая кривая подледно-подводной поверхности Земли",
abstract = "The distribution curvc of the heights and hypsographie curve of the Earth were compiled on the basis of the current data on the surface elevation and the bedrock topography of our planet. The dataset included the satellite data, bathymetry data for the World Ocean and the bedrock topography of Greenland and Antarctica - the most important glacicrs of our planet. The results show that taking into account the icc cover has a significant impact on the shape of the curvcs The greatest differences arc in the ranges of heights between 1500 and 4000 m and between -1000 and -200 m. According to calculations, the average altitude of the land surface and the stone surface is 800 m and 605 m, respectively.",
keywords = "Bedrock of the earth, Earth surfacc elevation, Hypsographie curvc",
author = "Попов, {Сергей Викторович}",
year = "2015",
doi = "10.15356/0435-4281-2015-4-85-90",
language = "русский",
pages = "85--90",
journal = "ГЕОМОРФОЛОГИЯ",
issn = "0435-4281",
publisher = "Российская академия наук",
number = "4",

}

RIS

TY - JOUR

T1 - Гипсографическая кривая подледно-подводной поверхности Земли

AU - Попов, Сергей Викторович

PY - 2015

Y1 - 2015

N2 - The distribution curvc of the heights and hypsographie curve of the Earth were compiled on the basis of the current data on the surface elevation and the bedrock topography of our planet. The dataset included the satellite data, bathymetry data for the World Ocean and the bedrock topography of Greenland and Antarctica - the most important glacicrs of our planet. The results show that taking into account the icc cover has a significant impact on the shape of the curvcs The greatest differences arc in the ranges of heights between 1500 and 4000 m and between -1000 and -200 m. According to calculations, the average altitude of the land surface and the stone surface is 800 m and 605 m, respectively.

AB - The distribution curvc of the heights and hypsographie curve of the Earth were compiled on the basis of the current data on the surface elevation and the bedrock topography of our planet. The dataset included the satellite data, bathymetry data for the World Ocean and the bedrock topography of Greenland and Antarctica - the most important glacicrs of our planet. The results show that taking into account the icc cover has a significant impact on the shape of the curvcs The greatest differences arc in the ranges of heights between 1500 and 4000 m and between -1000 and -200 m. According to calculations, the average altitude of the land surface and the stone surface is 800 m and 605 m, respectively.

KW - Bedrock of the earth

KW - Earth surfacc elevation

KW - Hypsographie curvc

UR - http://www.scopus.com/inward/record.url?scp=84973163813&partnerID=8YFLogxK

U2 - 10.15356/0435-4281-2015-4-85-90

DO - 10.15356/0435-4281-2015-4-85-90

M3 - статья

AN - SCOPUS:84973163813

SP - 85

EP - 90

JO - ГЕОМОРФОЛОГИЯ

JF - ГЕОМОРФОЛОГИЯ

SN - 0435-4281

IS - 4

ER -

ID: 36670177