Preprints
https://doi.org/10.5194/egusphere-2022-1324
https://doi.org/10.5194/egusphere-2022-1324
07 Dec 2022
 | 07 Dec 2022

Missing sea-level rise in southeast Greenland during and since the Little Ice Age

Sarah Alice Woodroffe, Leanne Mary Wake, Kristian K. Kjeldsen, Natasha Louise Mary Barlow, Antony James Long, and Kurt Henrik Kjaer

Abstract. The Greenland Ice Sheet has been losing mass at an accelerating rate over the past two decades. Understanding ice mass and glacier changes during the preceding several hundred years, prior to geodetic measurements, is more difficult because evidence of past ice extent in many places was later overridden. Saltmarshes provide the only continuous records of Relative Sea Level (RSL) from close to the Greenland Ice Sheet that span the period of time during and since the Little Ice Age (LIA) and can be used to reconstruct ice mass gain and loss over recent centuries. Saltmarsh sediments collected at the mouth of Dronning Marie Dal, close to the Greenland Ice Sheet margin in southeast Greenland, record RSL changes over the past c. 300 years through changing sediment and diatom stratigraphy. These RSL changes record a combination of processes that are dominated by local/regional changes in Greenland Ice Sheet mass balance during this critical period that spans the maximum of the LIA and 20th Century warming. In the early part of the record (1725–1762 CE) the rate of RSL rise is higher than reconstructed from the closest isolation basin at Timmiarmiut, but between 1762–1880 CE the RSL rate is within the error range of rate of RSL change recorded in the isolation basin. RSL begins to slowly fall around 1880 CE and then accelerates since the 1990s, with a total amount of RSL fall of 0.08 ±0.1 m in the last 140 years. Modelled RSL, which takes into account contributions from post-LIA Greenland Ice Sheet Glacio-isostatic Adjustment (GIA), ongoing deglacial GIA, the global non-ice sheet glacial melt fingerprint, contributions from thermosteric effects, the Antarctic mass loss sea-level fingerprint and terrestrial water storage, over-predicts the amount of RSL fall since the end of the LIA by at least 0.5 m. The GIA signal caused by post-LIA Greenland Ice Sheet mass loss is by far the largest contributor to this modelled RSL, and error in its calculation can have a large impact on RSL predictions at Dronning Marie Dal. We cannot reconcile the modelled RSL and the saltmarsh observations, even when moving the termination of the LIA to 1800 CE and reducing the post-LIA Greenland mass loss signal by 30 %, and a ‘budget residual’ of +~2.5 mm/yr since the end of the LIA remains unexplained.

Journal article(s) based on this preprint

02 Aug 2023
Missing sea level rise in southeastern Greenland during and since the Little Ice Age
Sarah A. Woodroffe, Leanne M. Wake, Kristian K. Kjeldsen, Natasha L. M. Barlow, Antony J. Long, and Kurt H. Kjær
Clim. Past, 19, 1585–1606, https://doi.org/10.5194/cp-19-1585-2023,https://doi.org/10.5194/cp-19-1585-2023, 2023
Short summary

Sarah Alice Woodroffe et al.

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2022-1324', Robin Edwards, 10 Jan 2023
    • AC1: 'Reply on RC1', Sarah Woodroffe, 30 Mar 2023
  • RC2: 'Comment on egusphere-2022-1324', Udita Mukherjee, 23 Feb 2023
    • AC2: 'Reply on RC2', Sarah Woodroffe, 30 Mar 2023

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2022-1324', Robin Edwards, 10 Jan 2023
    • AC1: 'Reply on RC1', Sarah Woodroffe, 30 Mar 2023
  • RC2: 'Comment on egusphere-2022-1324', Udita Mukherjee, 23 Feb 2023
    • AC2: 'Reply on RC2', Sarah Woodroffe, 30 Mar 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (05 Apr 2023) by Alessio Rovere
AR by Sarah Woodroffe on behalf of the Authors (17 May 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (30 May 2023) by Alessio Rovere
AR by Sarah Woodroffe on behalf of the Authors (07 Jun 2023)  Manuscript 

Journal article(s) based on this preprint

02 Aug 2023
Missing sea level rise in southeastern Greenland during and since the Little Ice Age
Sarah A. Woodroffe, Leanne M. Wake, Kristian K. Kjeldsen, Natasha L. M. Barlow, Antony J. Long, and Kurt H. Kjær
Clim. Past, 19, 1585–1606, https://doi.org/10.5194/cp-19-1585-2023,https://doi.org/10.5194/cp-19-1585-2023, 2023
Short summary

Sarah Alice Woodroffe et al.

Sarah Alice Woodroffe et al.

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The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.

Short summary
Saltmarsh in SE Greenland records sea-level changes over the past 300 years in sediments and microfossils. The pattern is rising sea level until ~1880 CE and small sea-level fall since. This disagrees with modelled sea-level, which over-predicts sea-level fall by at least 0.5 m. This is the same even when allowing more time for and reducing the overall amount of Greenland ice sheet melt. Fitting the model to the data leaves ~2.5 mm/yr of unexplained sea-level rise in SE Greenland since ~1880 CE.