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North Atlantic weather regimes in δ18O of winter precipitation : isotopic fingerprint of the response in the atmospheric circulation after volcanic eruptions

GuðlaugsdÓttir, Hera; Sjolte, Jesper LU ; Sveinbjörnsdóttir, ÁrnÝ Erla; Werner, Martin and Steen-Larsen, Hans Christian (2019) In Tellus, Series B: Chemical and Physical Meteorology 71(1). p.1-19
Abstract

Equatorial volcanic eruptions are known to impact the atmospheric circulation on seasonal time scales through a strengthening of the stratospheric zonal winds followed by dynamic ocean-atmosphere coupling. This emerges as the positive phase of the North Atlantic Oscillation in the first 5 years after an eruption. In the North Atlantic, other modes of atmospheric circulation contribute to the climate variability but their response to volcanic eruptions has been less studied. We address this by retrieving the stable water isotopic fingerprint of the four major atmospheric circulation modes over the North Atlantic (Atlantic Ridge, Scandinavian Blocking and the negative and positive phases of the North Atlantic Oscillation (NAO − and NAO+))... (More)

Equatorial volcanic eruptions are known to impact the atmospheric circulation on seasonal time scales through a strengthening of the stratospheric zonal winds followed by dynamic ocean-atmosphere coupling. This emerges as the positive phase of the North Atlantic Oscillation in the first 5 years after an eruption. In the North Atlantic, other modes of atmospheric circulation contribute to the climate variability but their response to volcanic eruptions has been less studied. We address this by retrieving the stable water isotopic fingerprint of the four major atmospheric circulation modes over the North Atlantic (Atlantic Ridge, Scandinavian Blocking and the negative and positive phases of the North Atlantic Oscillation (NAO − and NAO+)) by using monthly precipitation data from Global Network of Isotopes in Precipitation (GNIP) and 500 mb geo-potential height from the 20th Century Reanalysis. The simulated stable isotopic pattern of each atmospheric circulation mode is further used to assess the retrieved pattern. We test if changes in the atmospheric circulation as well as moisture source conditions as a result of volcanic eruptions can be identified by analyzing the winter climate response after both equatorial and high-latitude North Hemispheric volcanic eruptions in data, reanalysis and simulations. We report of an NAO + mode in the first two years after equatorial eruptions followed by NAO − in year 3 due to a decrease in the meridional temperature gradient as a result of volcanic surface cooling. This emerges in both GNIP data as well as reanalysis. Although the detected response is stronger after equatorial eruptions compared to high latitude eruptions, our results show that the response after high latitude eruptions tend to emerge as NAO − in year 2 followed by NAO + in year 3–4.

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author
organization
publishing date
type
Contribution to journal
publication status
published
subject
keywords
North Atlantic climate variability, stable water isotopes, volcanic eruptions
in
Tellus, Series B: Chemical and Physical Meteorology
volume
71
issue
1
pages
19 pages
publisher
Taylor & Francis
external identifiers
  • scopus:85069459907
ISSN
0280-6509
DOI
10.1080/16000889.2019.1633848
language
English
LU publication?
yes
id
6dcb5f7a-4db3-4cc5-8902-6a4436e2bd2c
date added to LUP
2019-08-09 16:05:09
date last changed
2019-08-28 04:58:04
@article{6dcb5f7a-4db3-4cc5-8902-6a4436e2bd2c,
  abstract     = {<p>Equatorial volcanic eruptions are known to impact the atmospheric circulation on seasonal time scales through a strengthening of the stratospheric zonal winds followed by dynamic ocean-atmosphere coupling. This emerges as the positive phase of the North Atlantic Oscillation in the first 5 years after an eruption. In the North Atlantic, other modes of atmospheric circulation contribute to the climate variability but their response to volcanic eruptions has been less studied. We address this by retrieving the stable water isotopic fingerprint of the four major atmospheric circulation modes over the North Atlantic (Atlantic Ridge, Scandinavian Blocking and the negative and positive phases of the North Atlantic Oscillation (NAO − and NAO+)) by using monthly precipitation data from Global Network of Isotopes in Precipitation (GNIP) and 500 mb geo-potential height from the 20th Century Reanalysis. The simulated stable isotopic pattern of each atmospheric circulation mode is further used to assess the retrieved pattern. We test if changes in the atmospheric circulation as well as moisture source conditions as a result of volcanic eruptions can be identified by analyzing the winter climate response after both equatorial and high-latitude North Hemispheric volcanic eruptions in data, reanalysis and simulations. We report of an NAO + mode in the first two years after equatorial eruptions followed by NAO − in year 3 due to a decrease in the meridional temperature gradient as a result of volcanic surface cooling. This emerges in both GNIP data as well as reanalysis. Although the detected response is stronger after equatorial eruptions compared to high latitude eruptions, our results show that the response after high latitude eruptions tend to emerge as NAO − in year 2 followed by NAO + in year 3–4.</p>},
  author       = {GuðlaugsdÓttir, Hera and Sjolte, Jesper and Sveinbjörnsdóttir, ÁrnÝ Erla and Werner, Martin and Steen-Larsen, Hans Christian},
  issn         = {0280-6509},
  keyword      = {North Atlantic climate variability,stable water isotopes,volcanic eruptions},
  language     = {eng},
  month        = {07},
  number       = {1},
  pages        = {1--19},
  publisher    = {Taylor & Francis},
  series       = {Tellus, Series B: Chemical and Physical Meteorology},
  title        = {North Atlantic weather regimes in δ<sup>18</sup>O of winter precipitation : isotopic fingerprint of the response in the atmospheric circulation after volcanic eruptions},
  url          = {http://dx.doi.org/10.1080/16000889.2019.1633848},
  volume       = {71},
  year         = {2019},
}