Phase State of Precipitation as a Factor of Low Flow in the Yana and Indigirka River Basins

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Phase State of Precipitation as a Factor of Low Flow in the Yana and Indigirka River Basins. / Makarieva, O. M.; Nesterova, N. V.

в: Russian Meteorology and Hydrology, Том 45, № 4, 22.05.2020, стр. 276-282.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

BibTeX

@article{0d1c44309ec14462b0c89082de8bdca3,

title = "Phase State of Precipitation as a Factor of Low Flow in the Yana and Indigirka River Basins",

abstract = "The results of streamflow data analysis for 18mountain catchments in the Yana and Indigirka river basins (1966–2015)with the area from 16.6 to 89600 km2 are presented. Theaverage streamflow increased by 13 mm (54%) is September, by 1.5 mm(57%) in October, by 0.4 mm (59%) in November, and by 0.1 mm (80%) inDecember on 12, 11, 9, and 7 rivers, respectively. Basically, thestreamflow variations are manifested in the form of abrupt shifts during1991–1996. There is a decrease in precipitation in winter (by 8–13 mm)and the absence of significant changes in the other seasons. An increasein average annual air temperature by 2.0°C led to an increase in theamount of liquid precipitation and streamflow in September by about 12mm. The revealed dependences of monthly streamflow on the amount ofliquid precipitation in September for small catchments (as well as thesingle period (1991–1996), when the simultaneous variations in thesehydrometeorological parameters are observed) indicate that the phasestate of precipitation is the main factor of changes in the low flow forthe analyzed rivers.",

keywords = "Climate warming, Liquid and solid precipitation, Low flow increase",

author = "Makarieva, {O. M.} and Nesterova, {N. V.}",

note = "Publisher Copyright: {\textcopyright} 2020, Allerton Press, Inc.",

year = "2020",

month = may,

day = "22",

doi = "10.3103/S1068373920040081",

language = "English",

volume = "45",

pages = "276--282",

journal = "Russian Meteorology and Hydrology",

issn = "1068-3739",

publisher = "Allerton Press, Inc.",

number = "4",

}

RIS

TY - JOUR

T1 - Phase State of Precipitation as a Factor of Low Flow in the Yana and Indigirka River Basins

AU - Makarieva, O. M.

AU - Nesterova, N. V.

PY - 2020/5/22

Y1 - 2020/5/22

N2 - The results of streamflow data analysis for 18mountain catchments in the Yana and Indigirka river basins (1966–2015)with the area from 16.6 to 89600 km2 are presented. Theaverage streamflow increased by 13 mm (54%) is September, by 1.5 mm(57%) in October, by 0.4 mm (59%) in November, and by 0.1 mm (80%) inDecember on 12, 11, 9, and 7 rivers, respectively. Basically, thestreamflow variations are manifested in the form of abrupt shifts during1991–1996. There is a decrease in precipitation in winter (by 8–13 mm)and the absence of significant changes in the other seasons. An increasein average annual air temperature by 2.0°C led to an increase in theamount of liquid precipitation and streamflow in September by about 12mm. The revealed dependences of monthly streamflow on the amount ofliquid precipitation in September for small catchments (as well as thesingle period (1991–1996), when the simultaneous variations in thesehydrometeorological parameters are observed) indicate that the phasestate of precipitation is the main factor of changes in the low flow forthe analyzed rivers.

AB - The results of streamflow data analysis for 18mountain catchments in the Yana and Indigirka river basins (1966–2015)with the area from 16.6 to 89600 km2 are presented. Theaverage streamflow increased by 13 mm (54%) is September, by 1.5 mm(57%) in October, by 0.4 mm (59%) in November, and by 0.1 mm (80%) inDecember on 12, 11, 9, and 7 rivers, respectively. Basically, thestreamflow variations are manifested in the form of abrupt shifts during1991–1996. There is a decrease in precipitation in winter (by 8–13 mm)and the absence of significant changes in the other seasons. An increasein average annual air temperature by 2.0°C led to an increase in theamount of liquid precipitation and streamflow in September by about 12mm. The revealed dependences of monthly streamflow on the amount ofliquid precipitation in September for small catchments (as well as thesingle period (1991–1996), when the simultaneous variations in thesehydrometeorological parameters are observed) indicate that the phasestate of precipitation is the main factor of changes in the low flow forthe analyzed rivers.

KW - Climate warming

KW - Liquid and solid precipitation

KW - Low flow increase

UR - http://www.scopus.com/inward/record.url?scp=85087546794&partnerID=8YFLogxK

U2 - 10.3103/S1068373920040081

DO - 10.3103/S1068373920040081

M3 - Article

AN - SCOPUS:85087546794

VL - 45

SP - 276

EP - 282

JO - Russian Meteorology and Hydrology

JF - Russian Meteorology and Hydrology

SN - 1068-3739

IS - 4

ER -

ID: 87710124