Standard

Hydrometeorological changes in the North-East of Russia. / Nesterova, Nataliia; Makarieva, Olga; Zemlyanskova, Anastasiia.

в: E3S Web of Conferences, Том 163, 05010, 17.04.2020.

Результаты исследований: Научные публикации в периодических изданиях › статья в журнале по материалам конференции › Рецензирование

Harvard

Nesterova, N, Makarieva, O & Zemlyanskova, A 2020, 'Hydrometeorological changes in the North-East of Russia', E3S Web of Conferences, Том. 163, 05010. https://doi.org/10.1051/e3sconf/202016305010

APA

Nesterova, N., Makarieva, O., & Zemlyanskova, A. (2020). Hydrometeorological changes in the North-East of Russia. E3S Web of Conferences, 163, [05010]. https://doi.org/10.1051/e3sconf/202016305010

Vancouver

Nesterova N, Makarieva O, Zemlyanskova A. Hydrometeorological changes in the North-East of Russia. E3S Web of Conferences. 2020 Апр. 17;163. 05010. https://doi.org/10.1051/e3sconf/202016305010

Author

Nesterova, Nataliia ; Makarieva, Olga ; Zemlyanskova, Anastasiia. / Hydrometeorological changes in the North-East of Russia. в: E3S Web of Conferences. 2020 ; Том 163.

BibTeX

@article{5ba6221a37024f4486e930b8438a6396,
title = "Hydrometeorological changes in the North-East of Russia",
abstract = "The paper presents a comprehensive analysis of hydrometeorological changes at the river basins of the North-East of Russia for the period 1966-2015. Data from 61 meteorological stations showed an increase in the air temperature by an average of 2.3 °C and multidirectional changes in annual precipitation. Most stations are characterized by a significant negative trend of precipitation in winter and a positive annual trend of mixed and liquid precipitation with an increase in their share in autumn months. The presence of statistically significant positive streamflow trends in the autumn-winter period was established for 51 hydrological gauges. We hypothesize that the increase in the low flow is mainly due to the transition of precipitation type from solid to liquid and corresponding increase of runoff in September, continuing in the following months.",
author = "Nataliia Nesterova and Olga Makarieva and Anastasiia Zemlyanskova",
note = "Publisher Copyright: {\textcopyright} 2020 The Authors, published by EDP Sciences.; 4th Vinogradov Conference on Hydrology: from Learning to Worldview in Memory of Outstanding Russian Hydrologist Yury Vinogradov, VC 2020 ; Conference date: 20-03-2020 Through 27-03-2020",
year = "2020",
month = apr,
day = "17",
doi = "10.1051/e3sconf/202016305010",
language = "English",
volume = "163",
journal = "E3S Web of Conferences",
issn = "2555-0403",
publisher = "EDP Sciences",

}

RIS

TY - JOUR

T1 - Hydrometeorological changes in the North-East of Russia

AU - Nesterova, Nataliia

AU - Makarieva, Olga

AU - Zemlyanskova, Anastasiia

N1 - Publisher Copyright: © 2020 The Authors, published by EDP Sciences.

PY - 2020/4/17

Y1 - 2020/4/17

N2 - The paper presents a comprehensive analysis of hydrometeorological changes at the river basins of the North-East of Russia for the period 1966-2015. Data from 61 meteorological stations showed an increase in the air temperature by an average of 2.3 °C and multidirectional changes in annual precipitation. Most stations are characterized by a significant negative trend of precipitation in winter and a positive annual trend of mixed and liquid precipitation with an increase in their share in autumn months. The presence of statistically significant positive streamflow trends in the autumn-winter period was established for 51 hydrological gauges. We hypothesize that the increase in the low flow is mainly due to the transition of precipitation type from solid to liquid and corresponding increase of runoff in September, continuing in the following months.

AB - The paper presents a comprehensive analysis of hydrometeorological changes at the river basins of the North-East of Russia for the period 1966-2015. Data from 61 meteorological stations showed an increase in the air temperature by an average of 2.3 °C and multidirectional changes in annual precipitation. Most stations are characterized by a significant negative trend of precipitation in winter and a positive annual trend of mixed and liquid precipitation with an increase in their share in autumn months. The presence of statistically significant positive streamflow trends in the autumn-winter period was established for 51 hydrological gauges. We hypothesize that the increase in the low flow is mainly due to the transition of precipitation type from solid to liquid and corresponding increase of runoff in September, continuing in the following months.

UR - http://www.scopus.com/inward/record.url?scp=85085243475&partnerID=8YFLogxK

U2 - 10.1051/e3sconf/202016305010

DO - 10.1051/e3sconf/202016305010

M3 - Conference article

VL - 163

JO - E3S Web of Conferences

JF - E3S Web of Conferences

SN - 2555-0403

M1 - 05010

T2 - 4th Vinogradov Conference on Hydrology: from Learning to Worldview in Memory of Outstanding Russian Hydrologist Yury Vinogradov, VC 2020

Y2 - 20 March 2020 through 27 March 2020

ER -

ID: 89154557