Snow?Dust Storm: Unique case study from Iceland, March 6?7, 2013
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41330%2F15%3A69466" target="_blank" >RIV/60460709:41330/15:69466 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/67985831:_____/15:00443041
Výsledek na webu
<a href="http://dx.doi.org/10.1016/j.aeolia.2014.11.001" target="_blank" >http://dx.doi.org/10.1016/j.aeolia.2014.11.001</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.aeolia.2014.11.001" target="_blank" >10.1016/j.aeolia.2014.11.001</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Snow?Dust Storm: Unique case study from Iceland, March 6?7, 2013
Popis výsledku v původním jazyce
Iceland is an active dust source in the high-latitude cold region. About 50% of the annual dust events in the southern part of Iceland take place at sub-zero temperatures or in winter, when dust may be mixed with snow. We investigated one winter dust event that occurred in March 2013. It resulted in a several mm thick dark layer of dust deposited on snow. Dust was transported over 250 km causing impurities on snow in the capital of Iceland, Reykjavik. Max one-minute PM10 concentration measured in Kirkjubajarklaustur (20?50 km from the dust source) exceeded 6500 ?g m-3 while the mean (median) PM10 concentration during 24-h storm was 1281 (1170) ?g m-3. Dust concentrations during the dust deposition in Reykjavik were only about 100 ?g m-3, suggesting a rapid removal of the dust particles by snow during the transport. Dust sample taken from the snow top layer in Reykjavik after the storm showed that about 75% of the dust deposit was a volcanic glass with SiO2 ~45%, FeO ~14.5%, and TiO2 ~3
Název v anglickém jazyce
Snow?Dust Storm: Unique case study from Iceland, March 6?7, 2013
Popis výsledku anglicky
Iceland is an active dust source in the high-latitude cold region. About 50% of the annual dust events in the southern part of Iceland take place at sub-zero temperatures or in winter, when dust may be mixed with snow. We investigated one winter dust event that occurred in March 2013. It resulted in a several mm thick dark layer of dust deposited on snow. Dust was transported over 250 km causing impurities on snow in the capital of Iceland, Reykjavik. Max one-minute PM10 concentration measured in Kirkjubajarklaustur (20?50 km from the dust source) exceeded 6500 ?g m-3 while the mean (median) PM10 concentration during 24-h storm was 1281 (1170) ?g m-3. Dust concentrations during the dust deposition in Reykjavik were only about 100 ?g m-3, suggesting a rapid removal of the dust particles by snow during the transport. Dust sample taken from the snow top layer in Reykjavik after the storm showed that about 75% of the dust deposit was a volcanic glass with SiO2 ~45%, FeO ~14.5%, and TiO2 ~3
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DI - Znečištění a kontrola vzduchu
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2015
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Aeolian Research
ISSN
1875-9637
e-ISSN
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Svazek periodika
2015
Číslo periodika v rámci svazku
16
Stát vydavatele periodika
CZ - Česká republika
Počet stran výsledku
6
Strana od-do
69-74
Kód UT WoS článku
000351648200008
EID výsledku v databázi Scopus
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