Influence of Weather Conditions on Particulate Matter Suspension following the 2010 Eyjafjallajökull Volcanic Eruption

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41330%2F20%3A82294" target="_blank" >RIV/60460709:41330/20:82294 - isvavai.cz</a>

Výsledek na webu

<a href="https://journals.ametsoc.org/view/journals/eint/24/6/eiD200006.xml" target="_blank" >https://journals.ametsoc.org/view/journals/eint/24/6/eiD200006.xml</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1175/EI-D-20-0006.1" target="_blank" >10.1175/EI-D-20-0006.1</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Influence of Weather Conditions on Particulate Matter Suspension following the 2010 Eyjafjallajökull Volcanic Eruption

Popis výsledku v původním jazyce

The 2010 eruption of Eyjafjallajokull produced volcanic ash that was mostly deposited to the south and east of the volcano with the thickest deposits closest to the eruption vents. For months following the eruption there were numerous reports of resuspended volcanic ash made by weather observers on the ground. A saltation sensor (SENSIT) and an Optical Particle Counter (OPC) located on the southern side of Eyjafjallajokull measured post eruptive particulate matter (PM) saltation and suspension events, some of which were also observable by satellite imagery. During the fall winter following the eruption visible satellite images and the SENSIT show that PM measured by the OPC were only detected by the when winds had a northerly component, making the source on the slopes of Eyjafjallajokull. During the largest observed events, particles 10 um were suspended but measured in extremely low concentrations ( 1 particle cm3). The saltation measurements, however, show high concentrations of particles 100 micr

Název v anglickém jazyce

Influence of Weather Conditions on Particulate Matter Suspension following the 2010 Eyjafjallajökull Volcanic Eruption

Popis výsledku anglicky

The 2010 eruption of Eyjafjallajokull produced volcanic ash that was mostly deposited to the south and east of the volcano with the thickest deposits closest to the eruption vents. For months following the eruption there were numerous reports of resuspended volcanic ash made by weather observers on the ground. A saltation sensor (SENSIT) and an Optical Particle Counter (OPC) located on the southern side of Eyjafjallajokull measured post eruptive particulate matter (PM) saltation and suspension events, some of which were also observable by satellite imagery. During the fall winter following the eruption visible satellite images and the SENSIT show that PM measured by the OPC were only detected by the when winds had a northerly component, making the source on the slopes of Eyjafjallajokull. During the largest observed events, particles 10 um were suspended but measured in extremely low concentrations ( 1 particle cm3). The saltation measurements, however, show high concentrations of particles 100 micr

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10509 - Meteorology and atmospheric sciences

Projekt

—

Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2020

Kód důvěrnosti údajů

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

Název periodika

Earth Interactions

ISSN

1087-3562

e-ISSN

1087-3562

Svazek periodika

24

Číslo periodika v rámci svazku

6

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

16

Strana od-do

1-16

Kód UT WoS článku

000619280300001

EID výsledku v databázi Scopus

2-s2.0-85096783116