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
Autor*in: |
Donovan, Amy [verfasserIn] |
---|
Format: |
Artikel |
---|---|
Sprache: |
Englisch |
Erschienen: |
2023 |
---|
Schlagwörter: |
---|
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: |
---|
DOI / URN: |
10.1007/s11069-023-06114-7 |
---|
Katalog-ID: |
OLC2145531807 |
---|
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 |
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 |