HYDROLOGICAL REGIME OF ADYGINE LAKE, TIEN SHAN, KYRGYZSTAN

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F14%3A10282377" target="_blank" >RIV/00216208:11310/14:10282377 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

HYDROLOGICAL REGIME OF ADYGINE LAKE, TIEN SHAN, KYRGYZSTAN

Popis výsledku v původním jazyce

This article provides a detailed analysis of the hydrological regime of the Adygine glacial lake in Tien Shan, Kyrgyzstan, and of the specific factors which affect it. Glaciers of central Tien Shan are considered to be very sensitive indicators of climate change. The studied lake belongs to a system of relatively recently formed lakes situated near the front of the retreating glacier and is numbered amongst the potentially dangerous. The lake's water level and its dependence on the development of climatic conditions in the area were monitored in detail in 2007-2012. A substantial part of this paper is the evaluation of the inflow and outflow balance of the lake's basin. The results confirmed that the hydrological regime is glacial and exhibits its typical characteristics, such as a seasonal evolution of runoff delay or significant diurnal fluctuation of the lake's water level. During the monitored period, no major changes in annual lake level fluctuation were recorded.

Název v anglickém jazyce

HYDROLOGICAL REGIME OF ADYGINE LAKE, TIEN SHAN, KYRGYZSTAN

Popis výsledku anglicky

This article provides a detailed analysis of the hydrological regime of the Adygine glacial lake in Tien Shan, Kyrgyzstan, and of the specific factors which affect it. Glaciers of central Tien Shan are considered to be very sensitive indicators of climate change. The studied lake belongs to a system of relatively recently formed lakes situated near the front of the retreating glacier and is numbered amongst the potentially dangerous. The lake's water level and its dependence on the development of climatic conditions in the area were monitored in detail in 2007-2012. A substantial part of this paper is the evaluation of the inflow and outflow balance of the lake's basin. The results confirmed that the hydrological regime is glacial and exhibits its typical characteristics, such as a seasonal evolution of runoff delay or significant diurnal fluctuation of the lake's water level. During the monitored period, no major changes in annual lake level fluctuation were recorded.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DA - Hydrologie a limnologie

OECD FORD obor

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Projekt

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Návaznosti

S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2014

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Geografie. Sborník české geografické společnosti (Geography Journal of Czech Geographic Society)

ISSN

1212-0014

e-ISSN

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Svazek periodika

119

Číslo periodika v rámci svazku

4

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

21

Strana od-do

320-341

Kód UT WoS článku

000347360500002

EID výsledku v databázi Scopus

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