Insights into volcanic hazards and plume chemistry from multi-parameter observations: the eruptions of Fimmvörðuháls and Eyjafjallajökull (2010) and Holuhraun (2014–2015)

Abstract The eruptions of Eyjafjallajökull volcano in 2010 (including its initial effusive phase at Fimmvörðuháls and its later explosive phase from the central volcano) and Bárðarbunga volcano in 2014–2015 (at Holuhraun) were widely reported. Here, we report on complementary, interdisciplinary obse...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Donovan, Amy [verfasserIn] Pfeffer, Melissa Barnie, Talfan Sawyer, Georgina Roberts, Tjarda Bergsson, Baldur Ilyinskaya, Evgenia Peters, Nial Buisman, Iris Snorrason, Arní Tsanev, Vitchko Oppenheimer, Clive

Format:	Artikel
Sprache:	Englisch

Erschienen:	2023

Schlagwörter:	Volcanic gas hazard Volcanic gas monitoring Iceland Multi-parameter monitoring Volcanic plumes

Anmerkung:	© The Author(s) 2023

Übergeordnetes Werk:	Enthalten in: Natural hazards - Springer Netherlands, 1988, 119(2023), 1 vom: 19. Aug., Seite 463-495
Übergeordnetes Werk:	volume:119 ; year:2023 ; number:1 ; day:19 ; month:08 ; pages:463-495

Links:	Volltext

DOI / URN:	10.1007/s11069-023-06114-7

Katalog-ID:	OLC2145531807

Internformat


LEADER	01000naa a22002652 4500
001	OLC2145531807
003	DE-627
005	20240118105204.0
007	tu
008	240118s2023 xx \|\|\|\|\| 00\| \|\|eng c
024	7		\|a 10.1007/s11069-023-06114-7 \|2 doi
035			\|a (DE-627)OLC2145531807
035			\|a (DE-He213)s11069-023-06114-7-p
040			\|a DE-627 \|b ger \|c DE-627 \|e rakwb
041			\|a eng
082	0	4	\|a 550 \|q VZ
084			\|a 14 \|2 ssgn
100	1		\|a Donovan, Amy \|e verfasserin \|0 (orcid)0000-0003-3596-5294 \|4 aut
245	1	0	\|a Insights into volcanic hazards and plume chemistry from multi-parameter observations: the eruptions of Fimmvörðuháls and Eyjafjallajökull (2010) and Holuhraun (2014–2015)
264		1	\|c 2023
336			\|a Text \|b txt \|2 rdacontent
337			\|a ohne Hilfsmittel zu benutzen \|b n \|2 rdamedia
338			\|a Band \|b nc \|2 rdacarrier
500			\|a © The Author(s) 2023
520			\|a Abstract The eruptions of Eyjafjallajökull volcano in 2010 (including its initial effusive phase at Fimmvörðuháls and its later explosive phase from the central volcano) and Bárðarbunga volcano in 2014–2015 (at Holuhraun) were widely reported. Here, we report on complementary, interdisciplinary observations made of the eruptive gases and lavas that shed light on the processes and atmospheric impacts of the eruptions, and afford an intercomparison of contrasting eruptive styles and hazards. We find that (i) consistent with other authors, there are substantial differences in the gas composition between the eruptions; namely that the deeper stored Eyjafjallajökull magmas led to greater enrichment in Cl relative to S; (ii) lava field $ SO_{2} $ degassing was measured to be 5–20% of the total emissions during Holuhraun, and the lava emissions were enriched in Cl at both fissure eruptions—particularly Fimmvörðuháls; and (iii) BrO is produced in Icelandic plumes in spite of the low UV levels.
650		4	\|a Volcanic gas hazard
650		4	\|a Volcanic gas monitoring
650		4	\|a Iceland
650		4	\|a Multi-parameter monitoring
650		4	\|a Volcanic plumes
700	1		\|a Pfeffer, Melissa \|4 aut
700	1		\|a Barnie, Talfan \|4 aut
700	1		\|a Sawyer, Georgina \|4 aut
700	1		\|a Roberts, Tjarda \|4 aut
700	1		\|a Bergsson, Baldur \|4 aut
700	1		\|a Ilyinskaya, Evgenia \|4 aut
700	1		\|a Peters, Nial \|4 aut
700	1		\|a Buisman, Iris \|4 aut
700	1		\|a Snorrason, Arní \|4 aut
700	1		\|a Tsanev, Vitchko \|4 aut
700	1		\|a Oppenheimer, Clive \|4 aut
773	0	8	\|i Enthalten in \|t Natural hazards \|d Springer Netherlands, 1988 \|g 119(2023), 1 vom: 19. Aug., Seite 463-495 \|w (DE-627)131010271 \|w (DE-600)1088547-X \|w (DE-576)03285272X \|x 0921-030X \|7 nnns
773	1	8	\|g volume:119 \|g year:2023 \|g number:1 \|g day:19 \|g month:08 \|g pages:463-495
856	4	1	\|u https://doi.org/10.1007/s11069-023-06114-7 \|z lizenzpflichtig \|3 Volltext
912			\|a GBV_USEFLAG_A
912			\|a SYSFLAG_A
912			\|a GBV_OLC
912			\|a SSG-OLC-PHY
912			\|a SSG-OLC-MAT
912			\|a SSG-OPC-GGO
912			\|a SSG-OPC-MAT
951			\|a AR
952			\|d 119 \|j 2023 \|e 1 \|b 19 \|c 08 \|h 463-495

Indexfelder

author_variant	a d ad m p mp t b tb g s gs t r tr b b bb e i ei n p np i b ib a s as v t vt c o co
matchkey_str	article:0921030X:2023----::nihsnoocncaadadlmceityrmutprmtrbevtosheutosfimrhsnej
hierarchy_sort_str	2023
publishDate	2023
allfields	10.1007/s11069-023-06114-7 doi (DE-627)OLC2145531807 (DE-He213)s11069-023-06114-7-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Donovan, Amy verfasserin (orcid)0000-0003-3596-5294 aut Insights into volcanic hazards and plume chemistry from multi-parameter observations: the eruptions of Fimmvörðuháls and Eyjafjallajökull (2010) and Holuhraun (2014–2015) 2023 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2023 Abstract The eruptions of Eyjafjallajökull volcano in 2010 (including its initial effusive phase at Fimmvörðuháls and its later explosive phase from the central volcano) and Bárðarbunga volcano in 2014–2015 (at Holuhraun) were widely reported. Here, we report on complementary, interdisciplinary observations made of the eruptive gases and lavas that shed light on the processes and atmospheric impacts of the eruptions, and afford an intercomparison of contrasting eruptive styles and hazards. We find that (i) consistent with other authors, there are substantial differences in the gas composition between the eruptions; namely that the deeper stored Eyjafjallajökull magmas led to greater enrichment in Cl relative to S; (ii) lava field $ SO_{2} $ degassing was measured to be 5–20% of the total emissions during Holuhraun, and the lava emissions were enriched in Cl at both fissure eruptions—particularly Fimmvörðuháls; and (iii) BrO is produced in Icelandic plumes in spite of the low UV levels. Volcanic gas hazard Volcanic gas monitoring Iceland Multi-parameter monitoring Volcanic plumes Pfeffer, Melissa aut Barnie, Talfan aut Sawyer, Georgina aut Roberts, Tjarda aut Bergsson, Baldur aut Ilyinskaya, Evgenia aut Peters, Nial aut Buisman, Iris aut Snorrason, Arní aut Tsanev, Vitchko aut Oppenheimer, Clive aut Enthalten in Natural hazards Springer Netherlands, 1988 119(2023), 1 vom: 19. Aug., Seite 463-495 (DE-627)131010271 (DE-600)1088547-X (DE-576)03285272X 0921-030X nnns volume:119 year:2023 number:1 day:19 month:08 pages:463-495 https://doi.org/10.1007/s11069-023-06114-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-MAT SSG-OPC-GGO SSG-OPC-MAT AR 119 2023 1 19 08 463-495
spelling	10.1007/s11069-023-06114-7 doi (DE-627)OLC2145531807 (DE-He213)s11069-023-06114-7-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Donovan, Amy verfasserin (orcid)0000-0003-3596-5294 aut Insights into volcanic hazards and plume chemistry from multi-parameter observations: the eruptions of Fimmvörðuháls and Eyjafjallajökull (2010) and Holuhraun (2014–2015) 2023 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2023 Abstract The eruptions of Eyjafjallajökull volcano in 2010 (including its initial effusive phase at Fimmvörðuháls and its later explosive phase from the central volcano) and Bárðarbunga volcano in 2014–2015 (at Holuhraun) were widely reported. Here, we report on complementary, interdisciplinary observations made of the eruptive gases and lavas that shed light on the processes and atmospheric impacts of the eruptions, and afford an intercomparison of contrasting eruptive styles and hazards. We find that (i) consistent with other authors, there are substantial differences in the gas composition between the eruptions; namely that the deeper stored Eyjafjallajökull magmas led to greater enrichment in Cl relative to S; (ii) lava field $ SO_{2} $ degassing was measured to be 5–20% of the total emissions during Holuhraun, and the lava emissions were enriched in Cl at both fissure eruptions—particularly Fimmvörðuháls; and (iii) BrO is produced in Icelandic plumes in spite of the low UV levels. Volcanic gas hazard Volcanic gas monitoring Iceland Multi-parameter monitoring Volcanic plumes Pfeffer, Melissa aut Barnie, Talfan aut Sawyer, Georgina aut Roberts, Tjarda aut Bergsson, Baldur aut Ilyinskaya, Evgenia aut Peters, Nial aut Buisman, Iris aut Snorrason, Arní aut Tsanev, Vitchko aut Oppenheimer, Clive aut Enthalten in Natural hazards Springer Netherlands, 1988 119(2023), 1 vom: 19. Aug., Seite 463-495 (DE-627)131010271 (DE-600)1088547-X (DE-576)03285272X 0921-030X nnns volume:119 year:2023 number:1 day:19 month:08 pages:463-495 https://doi.org/10.1007/s11069-023-06114-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-MAT SSG-OPC-GGO SSG-OPC-MAT AR 119 2023 1 19 08 463-495
allfields_unstemmed	10.1007/s11069-023-06114-7 doi (DE-627)OLC2145531807 (DE-He213)s11069-023-06114-7-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Donovan, Amy verfasserin (orcid)0000-0003-3596-5294 aut Insights into volcanic hazards and plume chemistry from multi-parameter observations: the eruptions of Fimmvörðuháls and Eyjafjallajökull (2010) and Holuhraun (2014–2015) 2023 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2023 Abstract The eruptions of Eyjafjallajökull volcano in 2010 (including its initial effusive phase at Fimmvörðuháls and its later explosive phase from the central volcano) and Bárðarbunga volcano in 2014–2015 (at Holuhraun) were widely reported. Here, we report on complementary, interdisciplinary observations made of the eruptive gases and lavas that shed light on the processes and atmospheric impacts of the eruptions, and afford an intercomparison of contrasting eruptive styles and hazards. We find that (i) consistent with other authors, there are substantial differences in the gas composition between the eruptions; namely that the deeper stored Eyjafjallajökull magmas led to greater enrichment in Cl relative to S; (ii) lava field $ SO_{2} $ degassing was measured to be 5–20% of the total emissions during Holuhraun, and the lava emissions were enriched in Cl at both fissure eruptions—particularly Fimmvörðuháls; and (iii) BrO is produced in Icelandic plumes in spite of the low UV levels. Volcanic gas hazard Volcanic gas monitoring Iceland Multi-parameter monitoring Volcanic plumes Pfeffer, Melissa aut Barnie, Talfan aut Sawyer, Georgina aut Roberts, Tjarda aut Bergsson, Baldur aut Ilyinskaya, Evgenia aut Peters, Nial aut Buisman, Iris aut Snorrason, Arní aut Tsanev, Vitchko aut Oppenheimer, Clive aut Enthalten in Natural hazards Springer Netherlands, 1988 119(2023), 1 vom: 19. Aug., Seite 463-495 (DE-627)131010271 (DE-600)1088547-X (DE-576)03285272X 0921-030X nnns volume:119 year:2023 number:1 day:19 month:08 pages:463-495 https://doi.org/10.1007/s11069-023-06114-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-MAT SSG-OPC-GGO SSG-OPC-MAT AR 119 2023 1 19 08 463-495
allfieldsGer	10.1007/s11069-023-06114-7 doi (DE-627)OLC2145531807 (DE-He213)s11069-023-06114-7-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Donovan, Amy verfasserin (orcid)0000-0003-3596-5294 aut Insights into volcanic hazards and plume chemistry from multi-parameter observations: the eruptions of Fimmvörðuháls and Eyjafjallajökull (2010) and Holuhraun (2014–2015) 2023 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2023 Abstract The eruptions of Eyjafjallajökull volcano in 2010 (including its initial effusive phase at Fimmvörðuháls and its later explosive phase from the central volcano) and Bárðarbunga volcano in 2014–2015 (at Holuhraun) were widely reported. Here, we report on complementary, interdisciplinary observations made of the eruptive gases and lavas that shed light on the processes and atmospheric impacts of the eruptions, and afford an intercomparison of contrasting eruptive styles and hazards. We find that (i) consistent with other authors, there are substantial differences in the gas composition between the eruptions; namely that the deeper stored Eyjafjallajökull magmas led to greater enrichment in Cl relative to S; (ii) lava field $ SO_{2} $ degassing was measured to be 5–20% of the total emissions during Holuhraun, and the lava emissions were enriched in Cl at both fissure eruptions—particularly Fimmvörðuháls; and (iii) BrO is produced in Icelandic plumes in spite of the low UV levels. Volcanic gas hazard Volcanic gas monitoring Iceland Multi-parameter monitoring Volcanic plumes Pfeffer, Melissa aut Barnie, Talfan aut Sawyer, Georgina aut Roberts, Tjarda aut Bergsson, Baldur aut Ilyinskaya, Evgenia aut Peters, Nial aut Buisman, Iris aut Snorrason, Arní aut Tsanev, Vitchko aut Oppenheimer, Clive aut Enthalten in Natural hazards Springer Netherlands, 1988 119(2023), 1 vom: 19. Aug., Seite 463-495 (DE-627)131010271 (DE-600)1088547-X (DE-576)03285272X 0921-030X nnns volume:119 year:2023 number:1 day:19 month:08 pages:463-495 https://doi.org/10.1007/s11069-023-06114-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-MAT SSG-OPC-GGO SSG-OPC-MAT AR 119 2023 1 19 08 463-495
allfieldsSound	10.1007/s11069-023-06114-7 doi (DE-627)OLC2145531807 (DE-He213)s11069-023-06114-7-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Donovan, Amy verfasserin (orcid)0000-0003-3596-5294 aut Insights into volcanic hazards and plume chemistry from multi-parameter observations: the eruptions of Fimmvörðuháls and Eyjafjallajökull (2010) and Holuhraun (2014–2015) 2023 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2023 Abstract The eruptions of Eyjafjallajökull volcano in 2010 (including its initial effusive phase at Fimmvörðuháls and its later explosive phase from the central volcano) and Bárðarbunga volcano in 2014–2015 (at Holuhraun) were widely reported. Here, we report on complementary, interdisciplinary observations made of the eruptive gases and lavas that shed light on the processes and atmospheric impacts of the eruptions, and afford an intercomparison of contrasting eruptive styles and hazards. We find that (i) consistent with other authors, there are substantial differences in the gas composition between the eruptions; namely that the deeper stored Eyjafjallajökull magmas led to greater enrichment in Cl relative to S; (ii) lava field $ SO_{2} $ degassing was measured to be 5–20% of the total emissions during Holuhraun, and the lava emissions were enriched in Cl at both fissure eruptions—particularly Fimmvörðuháls; and (iii) BrO is produced in Icelandic plumes in spite of the low UV levels. Volcanic gas hazard Volcanic gas monitoring Iceland Multi-parameter monitoring Volcanic plumes Pfeffer, Melissa aut Barnie, Talfan aut Sawyer, Georgina aut Roberts, Tjarda aut Bergsson, Baldur aut Ilyinskaya, Evgenia aut Peters, Nial aut Buisman, Iris aut Snorrason, Arní aut Tsanev, Vitchko aut Oppenheimer, Clive aut Enthalten in Natural hazards Springer Netherlands, 1988 119(2023), 1 vom: 19. Aug., Seite 463-495 (DE-627)131010271 (DE-600)1088547-X (DE-576)03285272X 0921-030X nnns volume:119 year:2023 number:1 day:19 month:08 pages:463-495 https://doi.org/10.1007/s11069-023-06114-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-MAT SSG-OPC-GGO SSG-OPC-MAT AR 119 2023 1 19 08 463-495
language	English
source	Enthalten in Natural hazards 119(2023), 1 vom: 19. Aug., Seite 463-495 volume:119 year:2023 number:1 day:19 month:08 pages:463-495
sourceStr	Enthalten in Natural hazards 119(2023), 1 vom: 19. Aug., Seite 463-495 volume:119 year:2023 number:1 day:19 month:08 pages:463-495
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Volcanic gas hazard Volcanic gas monitoring Iceland Multi-parameter monitoring Volcanic plumes
dewey-raw	550
isfreeaccess_bool	false
container_title	Natural hazards
authorswithroles_txt_mv	Donovan, Amy @@aut@@ Pfeffer, Melissa @@aut@@ Barnie, Talfan @@aut@@ Sawyer, Georgina @@aut@@ Roberts, Tjarda @@aut@@ Bergsson, Baldur @@aut@@ Ilyinskaya, Evgenia @@aut@@ Peters, Nial @@aut@@ Buisman, Iris @@aut@@ Snorrason, Arní @@aut@@ Tsanev, Vitchko @@aut@@ Oppenheimer, Clive @@aut@@
publishDateDaySort_date	2023-08-19T00:00:00Z
hierarchy_top_id	131010271
dewey-sort	3550
id	OLC2145531807
language_de	englisch
fullrecord	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000naa a22002652 4500</leader><controlfield tag="001">OLC2145531807</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20240118105204.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">240118s2023 xx \|\|\|\|\| 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s11069-023-06114-7</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2145531807</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s11069-023-06114-7-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">14</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Donovan, Amy</subfield><subfield code="e">verfasserin</subfield><subfield code="0">(orcid)0000-0003-3596-5294</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Insights into volcanic hazards and plume chemistry from multi-parameter observations: the eruptions of Fimmvörðuháls and Eyjafjallajökull (2010) and Holuhraun (2014–2015)</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2023</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© The Author(s) 2023</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The eruptions of Eyjafjallajökull volcano in 2010 (including its initial effusive phase at Fimmvörðuháls and its later explosive phase from the central volcano) and Bárðarbunga volcano in 2014–2015 (at Holuhraun) were widely reported. Here, we report on complementary, interdisciplinary observations made of the eruptive gases and lavas that shed light on the processes and atmospheric impacts of the eruptions, and afford an intercomparison of contrasting eruptive styles and hazards. We find that (i) consistent with other authors, there are substantial differences in the gas composition between the eruptions; namely that the deeper stored Eyjafjallajökull magmas led to greater enrichment in Cl relative to S; (ii) lava field $ SO_{2} $ degassing was measured to be 5–20% of the total emissions during Holuhraun, and the lava emissions were enriched in Cl at both fissure eruptions—particularly Fimmvörðuháls; and (iii) BrO is produced in Icelandic plumes in spite of the low UV levels.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Volcanic gas hazard</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Volcanic gas monitoring</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Iceland</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Multi-parameter monitoring</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Volcanic plumes</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Pfeffer, Melissa</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Barnie, Talfan</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sawyer, Georgina</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Roberts, Tjarda</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Bergsson, Baldur</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Ilyinskaya, Evgenia</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Peters, Nial</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Buisman, Iris</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Snorrason, Arní</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Tsanev, Vitchko</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Oppenheimer, Clive</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Natural hazards</subfield><subfield code="d">Springer Netherlands, 1988</subfield><subfield code="g">119(2023), 1 vom: 19. Aug., Seite 463-495</subfield><subfield code="w">(DE-627)131010271</subfield><subfield code="w">(DE-600)1088547-X</subfield><subfield code="w">(DE-576)03285272X</subfield><subfield code="x">0921-030X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:119</subfield><subfield code="g">year:2023</subfield><subfield code="g">number:1</subfield><subfield code="g">day:19</subfield><subfield code="g">month:08</subfield><subfield code="g">pages:463-495</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s11069-023-06114-7</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHY</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-MAT</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-MAT</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">119</subfield><subfield code="j">2023</subfield><subfield code="e">1</subfield><subfield code="b">19</subfield><subfield code="c">08</subfield><subfield code="h">463-495</subfield></datafield></record></collection>
author	Donovan, Amy
spellingShingle	Donovan, Amy ddc 550 ssgn 14 misc Volcanic gas hazard misc Volcanic gas monitoring misc Iceland misc Multi-parameter monitoring misc Volcanic plumes Insights into volcanic hazards and plume chemistry from multi-parameter observations: the eruptions of Fimmvörðuháls and Eyjafjallajökull (2010) and Holuhraun (2014–2015)
authorStr	Donovan, Amy
ppnlink_with_tag_str_mv	@@773@@(DE-627)131010271
format	Article
dewey-ones	550 - Earth sciences
delete_txt_mv	keep
author_role	aut aut aut aut aut aut aut aut aut aut aut aut
collection	OLC
remote_str	false
illustrated	Not Illustrated
issn	0921-030X
topic_title	550 VZ 14 ssgn Insights into volcanic hazards and plume chemistry from multi-parameter observations: the eruptions of Fimmvörðuháls and Eyjafjallajökull (2010) and Holuhraun (2014–2015) Volcanic gas hazard Volcanic gas monitoring Iceland Multi-parameter monitoring Volcanic plumes
topic	ddc 550 ssgn 14 misc Volcanic gas hazard misc Volcanic gas monitoring misc Iceland misc Multi-parameter monitoring misc Volcanic plumes
topic_unstemmed	ddc 550 ssgn 14 misc Volcanic gas hazard misc Volcanic gas monitoring misc Iceland misc Multi-parameter monitoring misc Volcanic plumes
topic_browse	ddc 550 ssgn 14 misc Volcanic gas hazard misc Volcanic gas monitoring misc Iceland misc Multi-parameter monitoring misc Volcanic plumes
format_facet	Aufsätze Gedruckte Aufsätze
format_main_str_mv	Text Zeitschrift/Artikel
carriertype_str_mv	nc
hierarchy_parent_title	Natural hazards
hierarchy_parent_id	131010271
dewey-tens	550 - Earth sciences & geology
hierarchy_top_title	Natural hazards
isfreeaccess_txt	false
familylinks_str_mv	(DE-627)131010271 (DE-600)1088547-X (DE-576)03285272X
title	Insights into volcanic hazards and plume chemistry from multi-parameter observations: the eruptions of Fimmvörðuháls and Eyjafjallajökull (2010) and Holuhraun (2014–2015)
ctrlnum	(DE-627)OLC2145531807 (DE-He213)s11069-023-06114-7-p
title_full	Insights into volcanic hazards and plume chemistry from multi-parameter observations: the eruptions of Fimmvörðuháls and Eyjafjallajökull (2010) and Holuhraun (2014–2015)
author_sort	Donovan, Amy
journal	Natural hazards
journalStr	Natural hazards
lang_code	eng
isOA_bool	false
dewey-hundreds	500 - Science
recordtype	marc
publishDateSort	2023
contenttype_str_mv	txt
container_start_page	463
author_browse	Donovan, Amy Pfeffer, Melissa Barnie, Talfan Sawyer, Georgina Roberts, Tjarda Bergsson, Baldur Ilyinskaya, Evgenia Peters, Nial Buisman, Iris Snorrason, Arní Tsanev, Vitchko Oppenheimer, Clive
container_volume	119
class	550 VZ 14 ssgn
format_se	Aufsätze
author-letter	Donovan, Amy
doi_str_mv	10.1007/s11069-023-06114-7
normlink	(ORCID)0000-0003-3596-5294
normlink_prefix_str_mv	(orcid)0000-0003-3596-5294
dewey-full	550
title_sort	insights into volcanic hazards and plume chemistry from multi-parameter observations: the eruptions of fimmvörðuháls and eyjafjallajökull (2010) and holuhraun (2014–2015)
title_auth	Insights into volcanic hazards and plume chemistry from multi-parameter observations: the eruptions of Fimmvörðuháls and Eyjafjallajökull (2010) and Holuhraun (2014–2015)
abstract	Abstract The eruptions of Eyjafjallajökull volcano in 2010 (including its initial effusive phase at Fimmvörðuháls and its later explosive phase from the central volcano) and Bárðarbunga volcano in 2014–2015 (at Holuhraun) were widely reported. Here, we report on complementary, interdisciplinary observations made of the eruptive gases and lavas that shed light on the processes and atmospheric impacts of the eruptions, and afford an intercomparison of contrasting eruptive styles and hazards. We find that (i) consistent with other authors, there are substantial differences in the gas composition between the eruptions; namely that the deeper stored Eyjafjallajökull magmas led to greater enrichment in Cl relative to S; (ii) lava field $ SO_{2} $ degassing was measured to be 5–20% of the total emissions during Holuhraun, and the lava emissions were enriched in Cl at both fissure eruptions—particularly Fimmvörðuháls; and (iii) BrO is produced in Icelandic plumes in spite of the low UV levels. © The Author(s) 2023
abstractGer	Abstract The eruptions of Eyjafjallajökull volcano in 2010 (including its initial effusive phase at Fimmvörðuháls and its later explosive phase from the central volcano) and Bárðarbunga volcano in 2014–2015 (at Holuhraun) were widely reported. Here, we report on complementary, interdisciplinary observations made of the eruptive gases and lavas that shed light on the processes and atmospheric impacts of the eruptions, and afford an intercomparison of contrasting eruptive styles and hazards. We find that (i) consistent with other authors, there are substantial differences in the gas composition between the eruptions; namely that the deeper stored Eyjafjallajökull magmas led to greater enrichment in Cl relative to S; (ii) lava field $ SO_{2} $ degassing was measured to be 5–20% of the total emissions during Holuhraun, and the lava emissions were enriched in Cl at both fissure eruptions—particularly Fimmvörðuháls; and (iii) BrO is produced in Icelandic plumes in spite of the low UV levels. © The Author(s) 2023
abstract_unstemmed	Abstract The eruptions of Eyjafjallajökull volcano in 2010 (including its initial effusive phase at Fimmvörðuháls and its later explosive phase from the central volcano) and Bárðarbunga volcano in 2014–2015 (at Holuhraun) were widely reported. Here, we report on complementary, interdisciplinary observations made of the eruptive gases and lavas that shed light on the processes and atmospheric impacts of the eruptions, and afford an intercomparison of contrasting eruptive styles and hazards. We find that (i) consistent with other authors, there are substantial differences in the gas composition between the eruptions; namely that the deeper stored Eyjafjallajökull magmas led to greater enrichment in Cl relative to S; (ii) lava field $ SO_{2} $ degassing was measured to be 5–20% of the total emissions during Holuhraun, and the lava emissions were enriched in Cl at both fissure eruptions—particularly Fimmvörðuháls; and (iii) BrO is produced in Icelandic plumes in spite of the low UV levels. © The Author(s) 2023
collection_details	GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-MAT SSG-OPC-GGO SSG-OPC-MAT
container_issue	1
title_short	Insights into volcanic hazards and plume chemistry from multi-parameter observations: the eruptions of Fimmvörðuháls and Eyjafjallajökull (2010) and Holuhraun (2014–2015)
url	https://doi.org/10.1007/s11069-023-06114-7
remote_bool	false
author2	Pfeffer, Melissa Barnie, Talfan Sawyer, Georgina Roberts, Tjarda Bergsson, Baldur Ilyinskaya, Evgenia Peters, Nial Buisman, Iris Snorrason, Arní Tsanev, Vitchko Oppenheimer, Clive
author2Str	Pfeffer, Melissa Barnie, Talfan Sawyer, Georgina Roberts, Tjarda Bergsson, Baldur Ilyinskaya, Evgenia Peters, Nial Buisman, Iris Snorrason, Arní Tsanev, Vitchko Oppenheimer, Clive
ppnlink	131010271
mediatype_str_mv	n
isOA_txt	false
hochschulschrift_bool	false
doi_str	10.1007/s11069-023-06114-7
up_date	2024-07-04T03:29:29.116Z
_version_	1803617586771918848
fullrecord_marcxml	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000naa a22002652 4500</leader><controlfield tag="001">OLC2145531807</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20240118105204.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">240118s2023 xx \|\|\|\|\| 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s11069-023-06114-7</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2145531807</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s11069-023-06114-7-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">14</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Donovan, Amy</subfield><subfield code="e">verfasserin</subfield><subfield code="0">(orcid)0000-0003-3596-5294</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Insights into volcanic hazards and plume chemistry from multi-parameter observations: the eruptions of Fimmvörðuháls and Eyjafjallajökull (2010) and Holuhraun (2014–2015)</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2023</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© The Author(s) 2023</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The eruptions of Eyjafjallajökull volcano in 2010 (including its initial effusive phase at Fimmvörðuháls and its later explosive phase from the central volcano) and Bárðarbunga volcano in 2014–2015 (at Holuhraun) were widely reported. Here, we report on complementary, interdisciplinary observations made of the eruptive gases and lavas that shed light on the processes and atmospheric impacts of the eruptions, and afford an intercomparison of contrasting eruptive styles and hazards. We find that (i) consistent with other authors, there are substantial differences in the gas composition between the eruptions; namely that the deeper stored Eyjafjallajökull magmas led to greater enrichment in Cl relative to S; (ii) lava field $ SO_{2} $ degassing was measured to be 5–20% of the total emissions during Holuhraun, and the lava emissions were enriched in Cl at both fissure eruptions—particularly Fimmvörðuháls; and (iii) BrO is produced in Icelandic plumes in spite of the low UV levels.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Volcanic gas hazard</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Volcanic gas monitoring</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Iceland</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Multi-parameter monitoring</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Volcanic plumes</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Pfeffer, Melissa</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Barnie, Talfan</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sawyer, Georgina</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Roberts, Tjarda</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Bergsson, Baldur</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Ilyinskaya, Evgenia</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Peters, Nial</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Buisman, Iris</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Snorrason, Arní</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Tsanev, Vitchko</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Oppenheimer, Clive</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Natural hazards</subfield><subfield code="d">Springer Netherlands, 1988</subfield><subfield code="g">119(2023), 1 vom: 19. Aug., Seite 463-495</subfield><subfield code="w">(DE-627)131010271</subfield><subfield code="w">(DE-600)1088547-X</subfield><subfield code="w">(DE-576)03285272X</subfield><subfield code="x">0921-030X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:119</subfield><subfield code="g">year:2023</subfield><subfield code="g">number:1</subfield><subfield code="g">day:19</subfield><subfield code="g">month:08</subfield><subfield code="g">pages:463-495</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s11069-023-06114-7</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHY</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-MAT</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-MAT</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">119</subfield><subfield code="j">2023</subfield><subfield code="e">1</subfield><subfield code="b">19</subfield><subfield code="c">08</subfield><subfield code="h">463-495</subfield></datafield></record></collection>
score	7.401268

Nicht das Richtige dabei?

Schreiben Sie uns!

Insights into volcanic hazards and plume chemistry from multi-parameter observations: the eruptions of Fimmvörðuháls and Eyjafjallajökull (2010) and Holuhraun (2014–2015)

Nicht das Richtige dabei?

Zugang & Verfügbarkeit

Vorhandene Bände

Nicht das Richtige dabei?