Preprints
https://doi.org/10.5194/essd-2021-170
https://doi.org/10.5194/essd-2021-170

  25 May 2021

25 May 2021

Review status: this discussion paper is a preprint. It has been under review for the journal Earth System Science Data (ESSD). The manuscript was not accepted for further review after discussion.

Sea surface height anomaly and geostrophic velocity from altimetry measurements over the Arctic Ocean (2011–2018)

Francesca Doglioni1, Robert Ricker1, Benjamin Rabe1, and Torsten Kanzow1,2 Francesca Doglioni et al.
  • 1Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany
  • 2Department 1 of Physics and Electrical Engeneering, Universität Bremen, Germany

Abstract. In recent decades the decline of the Arctic sea ice has modified vertical momentum fluxes from the atmosphere to the ice and the ocean, thereby affecting the surface circulation. In the past ten years satellite altimetry has contributed to understand these changes. However, data from ice-covered regions require dedicated processing, originating inconsistency between ice-covered and open ocean regions in terms of biases, corrections and data coverage. Thus, efforts to generate consistent Arctic-wide datasets are still required to enable the study of the Arctic Ocean surface circulation at basin-wide scales. Here we provide and assess a monthly gridded dataset of sea surface height anomaly and geostrophic velocity. This dataset is based on Cryosat-2 observations over ice-covered and open ocean areas of the Arctic up to 88° N for the period 2011 to 2018, interpolated using the Data-Interpolating Variational Analysis (DIVA) method. Geostrophic velocity was not available north of 82° N before this study. To examine the robustness of our results, we compare the generated fields to one independent altimetry dataset and independent data of ocean bottom pressure, steric height and near-surface ocean velocity from moorings. Results from the comparison to near-surface ocean velocity show that our geostrophic velocity fields can resolve seasonal to interannual variability of boundary currents wider than about 50 km. We further discuss the seasonal cycle of sea surface height and geostrophic velocity in the context of previous literature. Large scale features emerge, i.e. Arctic-wide maximum sea surface height between October and January, with the highest amplitude over the shelves, and basin wide seasonal acceleration of Arctic slope currents in winter. We suggest that this dataset can be used to study not only the large scale sea surface height and circulation but also the regionally confined boundary currents. The dataset is available in netCDF format from PANGAEA at [data currently under review].

Francesca Doglioni et al.

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on essd-2021-170', Anonymous Referee #1, 01 Jul 2021
  • RC2: 'Comment on essd-2021-170', James Morison, 17 Jul 2021

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on essd-2021-170', Anonymous Referee #1, 01 Jul 2021
  • RC2: 'Comment on essd-2021-170', James Morison, 17 Jul 2021

Francesca Doglioni et al.

Data sets

Acoustic Dopper Current Profiler (ADCP) from moorings taken in the Eurasian and Makarov basins, Arctic Ocean, 2015–2018. Arctic Data Center Igor Polyakov https://doi.org/10.18739/A2HT2GB80

Physical oceanography and current meter data (including raw data) from FRAM moorings in the Fram Strait, 2016–2018 von Appen, Wilken-Jon https://doi.org/10.1594/PANGAEA.904565

NABOS II – ADCP Water Current Data 2013–2015. urn:node:ARCTIC Igor Polyakov https://doi.org/10.18739/A28G8FJ3H

Physical oceanography and current meter data from moorings F1-F14 and F15/F16 in the Fram Strait, 1997–2016 von Appen, Wilken-Jon; Beszczynska-Möller, Agnieszka; Schauer, Ursula; Fahrbach, Eberhard https://doi.org/10.1594/PANGAEA.900883

Francesca Doglioni et al.

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Short summary
This paper presents a new satellite-derived gridded dataset of sea surface height and geostrophic velocity, over the Arctic ice-covered and ice-free regions up to 88° N. The dataset includes velocities north of 82° N, which were not available before. We assess the dataset by comparison to one independent satellite dataset and to independent mooring data. Results show that the geostrophic velocity fields can resolve seasonal to interannual variability of boundary currents wider than about 50 km.