Volcanic stratospheric sulfur injections and aerosol optical depth during the Holocene (past 11 500 years) from a bipolar ice-core array

to related objects

Abstract + 16  %) and cumulative VSSI (+ 86  %) compared with the past 2500 years. This increase coincides with the rapid retreat of ice sheets during deglaciation, providing context for potential future increases in volcanic activity in regions under projected glacier melting in the 21st century. The reconstructed VSSI and SAOD data are available at 10.1594/PANGAEA.928646 (Sigl et al., 2021).

Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: Online-Ressource

Language: Englisch

Bibliographic citation: Volcanic stratospheric sulfur injections and aerosol optical depth during the Holocene (past 11 500 years) from a bipolar ice-core array ; volume:14 ; number:7 ; year:2022 ; pages:3167-3196 ; extent:30
Earth system science data ; 14, Heft 7 (2022), 3167-3196 (gesamt 30)

Creator: Sigl, Michael
Toohey, Matthew
McConnell, Joseph R.
Cole-Dai, Jihong
Severi, Mirko

DOI: 10.5194/essd-14-3167-2022

URN: urn:nbn:de:101:1-2022071405175227306336

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 15.08.2025, 7:34 AM CEST

Data provider

This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.

Show original at data provider

Associated

Sigl, Michael
Toohey, Matthew
McConnell, Joseph R.
Cole-Dai, Jihong
Severi, Mirko

Other Objects (12)

Volcanic stratospheric injections up to 160 Tg (S) yield a Eurasian winter warming indistinguishable from internal variability

Volcanic stratospheric injections up to 160 Tg (S) yield a Eurasian winter warming indistinguishable from internal variability

High-resolution stratospheric volcanic SO2 injections in WACCM

High-resolution stratospheric volcanic SO<sub>2</sub> injections in WACCM

Volcanic stratospheric sulfur injections and aerosol optical depth during the Holocene (past 11,500 years) from a bipolar ice core array

Volcanic stratospheric sulfur injections and aerosol optical depth during the Holocene (past 11,500 years) from a bipolar ice core array

Volcanic stratospheric sulphur injections and aerosol optical depth from 500 BCE to 1900 CE

Volcanic stratospheric sulphur injections and aerosol optical depth from 500 BCE to 1900 CE

Volcanic stratospheric sulfur injections and aerosol optical depth from 500 BCE to 1900 CE

Volcanic stratospheric sulfur injections and aerosol optical depth from 500 BCE to 1900 CE

Volcanic stratospheric injections up to 160 Tg (S) yield a Eurasian winter warming indistinguishable from internal variability

Volcanic stratospheric injections up to 160 Tg (S) yield a Eurasian winter warming indistinguishable from internal variability

Stratospheric aerosol size reduction after volcanic eruptions

Stratospheric aerosol size reduction after volcanic eruptions

Stratospheric aerosol size reduction after volcanic eruptions

Stratospheric aerosol size reduction after volcanic eruptions

PalVol v1: a proxy-based semi-stochastic ensemble reconstruction of volcanic stratospheric sulfur injection for the last glacial cycle (140 000–50 BP)

PalVol v1: a proxy-based semi-stochastic ensemble reconstruction of volcanic stratospheric sulfur injection for the last glacial cycle (140 000–50 BP)

Reaching 1.5 °C and 2.0 °C global surface temperature targets using stratospheric aerosol geoengineering

Reaching 1.5 °C and 2.0 °C global surface temperature targets using stratospheric aerosol geoengineering

High latitude Southern Hemisphere fire history during the Mid-Late Holocene (750–6000 yr BP)

High latitude Southern Hemisphere fire history during the Mid-Late Holocene (750–6000 yr BP)

Volcanic influence on centennial to millennial Holocene Greenland temperature change

Volcanic influence on centennial to millennial Holocene Greenland temperature change

Volcanic stratospheric injections up to 160 Tg (S) yield a Eurasian winter warming indistinguishable from internal variability

Volcanic stratospheric injections up to 160 Tg (S) yield a Eurasian winter warming indistinguishable from internal variability

High-resolution stratospheric volcanic SO2 injections in WACCM

High-resolution stratospheric volcanic SO<sub>2</sub> injections in WACCM

Volcanic stratospheric sulfur injections and aerosol optical depth during the Holocene (past 11,500 years) from a bipolar ice core array

Volcanic stratospheric sulfur injections and aerosol optical depth during the Holocene (past 11,500 years) from a bipolar ice core array

Volcanic stratospheric sulphur injections and aerosol optical depth from 500 BCE to 1900 CE

Volcanic stratospheric sulphur injections and aerosol optical depth from 500 BCE to 1900 CE

Volcanic stratospheric sulfur injections and aerosol optical depth from 500 BCE to 1900 CE

Volcanic stratospheric sulfur injections and aerosol optical depth from 500 BCE to 1900 CE

Volcanic stratospheric injections up to 160 Tg (S) yield a Eurasian winter warming indistinguishable from internal variability

Volcanic stratospheric injections up to 160 Tg (S) yield a Eurasian winter warming indistinguishable from internal variability

Stratospheric aerosol size reduction after volcanic eruptions

Stratospheric aerosol size reduction after volcanic eruptions

Stratospheric aerosol size reduction after volcanic eruptions

Stratospheric aerosol size reduction after volcanic eruptions

PalVol v1: a proxy-based semi-stochastic ensemble reconstruction of volcanic stratospheric sulfur injection for the last glacial cycle (140 000–50 BP)

PalVol v1: a proxy-based semi-stochastic ensemble reconstruction of volcanic stratospheric sulfur injection for the last glacial cycle (140 000–50 BP)

Reaching 1.5 °C and 2.0 °C global surface temperature targets using stratospheric aerosol geoengineering

Reaching 1.5 °C and 2.0 °C global surface temperature targets using stratospheric aerosol geoengineering

High latitude Southern Hemisphere fire history during the Mid-Late Holocene (750–6000 yr BP)

High latitude Southern Hemisphere fire history during the Mid-Late Holocene (750–6000 yr BP)

Volcanic influence on centennial to millennial Holocene Greenland temperature change

Volcanic influence on centennial to millennial Holocene Greenland temperature change

Volcanic stratospheric injections up to 160 Tg (S) yield a Eurasian winter warming indistinguishable from internal variability

Volcanic stratospheric injections up to 160 Tg (S) yield a Eurasian winter warming indistinguishable from internal variability

High-resolution stratospheric volcanic SO2 injections in WACCM

High-resolution stratospheric volcanic SO<sub>2</sub> injections in WACCM

Volcanic stratospheric sulfur injections and aerosol optical depth during the Holocene (past 11,500 years) from a bipolar ice core array

Volcanic stratospheric sulfur injections and aerosol optical depth during the Holocene (past 11,500 years) from a bipolar ice core array

Volcanic stratospheric sulphur injections and aerosol optical depth from 500 BCE to 1900 CE

Volcanic stratospheric sulphur injections and aerosol optical depth from 500 BCE to 1900 CE

Volcanic stratospheric sulfur injections and aerosol optical depth from 500 BCE to 1900 CE

Volcanic stratospheric sulfur injections and aerosol optical depth from 500 BCE to 1900 CE

Volcanic stratospheric injections up to 160 Tg (S) yield a Eurasian winter warming indistinguishable from internal variability

Volcanic stratospheric injections up to 160 Tg (S) yield a Eurasian winter warming indistinguishable from internal variability

Stratospheric aerosol size reduction after volcanic eruptions

Stratospheric aerosol size reduction after volcanic eruptions

Stratospheric aerosol size reduction after volcanic eruptions

Stratospheric aerosol size reduction after volcanic eruptions

PalVol v1: a proxy-based semi-stochastic ensemble reconstruction of volcanic stratospheric sulfur injection for the last glacial cycle (140 000–50 BP)

PalVol v1: a proxy-based semi-stochastic ensemble reconstruction of volcanic stratospheric sulfur injection for the last glacial cycle (140 000–50 BP)

Reaching 1.5 °C and 2.0 °C global surface temperature targets using stratospheric aerosol geoengineering

Reaching 1.5 °C and 2.0 °C global surface temperature targets using stratospheric aerosol geoengineering

High latitude Southern Hemisphere fire history during the Mid-Late Holocene (750–6000 yr BP)

High latitude Southern Hemisphere fire history during the Mid-Late Holocene (750–6000 yr BP)

Volcanic influence on centennial to millennial Holocene Greenland temperature change

Volcanic influence on centennial to millennial Holocene Greenland temperature change

Cultural heritage institutions wishing to register will find more information here.

Fields marked * need to be filled in.

Username*

Please enter your username

Email*

Please enter your email address

Please do not fill this field

First name

Last name

Password*

Please enter your password

Confirm password*

Please enter the same password

I have read the terms of use and the privacy policy for the collection of personal data and accept them. *

This field is required.

I would like to subscribe to the newsletter of the Deutsche Digitale Bibliothek. See newsletter subscription info.

Account created

Your "My DDB" account has been successfully created. Before you can log in to your account, you must click the confirmation link in the message we just sent to the email address you provided.