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Amundsen Sea Low indices

The Amundsen Sea Low (ASL) is a climatological low pressure center located over the extreme southern Pacific Ocean, off the coast of West Antarctica.  Atmospheric variability in this region is larger than anywhere else in the Southern Hemisphere, and exhibits significant correlations with both the Southern Annular Mode (SAM) and ENSO.  Given its linkages to basin-wide ENSO variability, the ASL may be thought of as a Southern Hemisphere analog to the Aleutian Low (see North Pacific Index).  The ASL plays a significant role in the climate variability of West Antarctica and the adjacent oceanic environment.  Due to the extreme variability in the ASL region, and the seasonal migration of the ASL's low-pressure center, defining a single index of the ASL is challenging.  A consistent set of indices of the ASL, including its absolute and relative central pressure, and the latitude and longitude of these central pressures, has been derived from the ECMWF reanalysis.  The term Amundsen-Bellingshausen Seas Low (ABSL) is another name for the ASL.

Key Strengths:

  • Captures a large fraction of atmospheric variability in the most dynamic region of the Southern Hemisphere
  • Correlates with anomalies in winds, sea ice, air temperatures and other variables, giving confidence in its robustness and relevance to regional climate variability

Key Limitations:

  • Difficult to quantify the strength of the ASL due to large background variability
  • Short record length due to limited observations and the lack of long-term, reliable atmospheric reanalysis
  • Few in-situ data available to assess the reliability of the ASL indices; spurious variability and trends could arise from the use of atmospheric reanalysis

Expert Developer Guidance

The following was contributed by Dr. Scott Hosking of the British Antarctic Survey, January, 2016 (updated 14 Janurary 2020):

The Amundsen Sea Low is a climatological low pressure system located in the Pacific sector of the Southern Ocean. In this sector, variability in sea-level pressure is greater than anywhere in the Southern Hemisphere making it challenging to isolate local fluctuations in the ASL from larger- scale shifts in atmospheric pressure. The position and strength of the ASL are key drivers of regional change over West Antarctica (Hosking et al., 2013; Coggins and McDonald, 2015).

There has been much recent interest in the ASL because (i) rapid retreat of Pine Island and Thwaites glaciers (McMillan et al, 2015), (ii) observed rapid warming over central West Antarctica (Bromwich et al., 2012), and (iii) increase in snowfall in coastal West Antarctica (Thomas et al., 2015).

Version 2 differs slightly from that described in Hosking et al. [2013] which defined the location of the ASL as the point of lowest central pressure within the ASL sector region. This updated methodology ensures that the ASL is not falsely identified in cases where there is no local minima within the defined boundaries (as is the case in some CMIP5 models). In any case, when applied to the ERA-Interim reanalysis the results are relatively insensitive to the ASL detection method employed.

The dataset website https://www.bas.ac.uk/data/absl/ has monthly, seasonal and annual data. Note that the seasonal and annual indices are computed from their respective temporally averaged two-dimensional surface pressure fields. They are not the average of the three (or twelve) points from the monthly indices. ##

Years of Record

1979/01 to 2020/01
temporal metadataID:

Formats

Timestep

Monthly | Seasonal | Annual

Domain

Antarctic | SH - Southern Hemisphere | Southern Ocean

Vertical Levels

Surface Data Set

Input Data

ECMWF reanalysis

Earth system components and main variables

Atmosphere, Sea Level Pressure

Suggested Data Citation

 

Data Access: Please Cite data sources, following the data providers' instructions.

  1. Hosking's ASL Index page (monthly, seasonal, annual)

  1. Bromwich, D. H., J. P. Nicolas, A. J. Monaghan, M. A. Lazzara, L. M. Keller, G. A. Weidner, and A. B. Wilson (2012), Central West Antarctica among the most rapidly warming regions on Earth, Nat. Geosci., 6(2), 139–145, doi:10.1038/ngeo1671.
  2. Coggins, J. H. J., and A. J. McDonald (2015), The influence of the Amundsen Sea Low on the winds in the Ross Sea and surroundings: Insights from a synoptic climatology, J. Geophys. Res. Atmos. , 120 , 2167–2189, doi:10.1002/2014JD022830.
  3. Freeland, S. L., and B. N. Handy (1998), Data analysis with the SolarSoft system, Sol. Phys., 182(2), 497–500, doi:10.1023/A:1005038224881.
  4. Hosking, J. S., A. Orr, T. J. Bracegirdle, and J. Turner (2016), Future circulation changes off West Antarctica: Sensitivity of the Amundsen Sea Low to projected anthropogenic forcing, Geophys. Res. Lett., 43, doi:10.1002/2015GL067143.
  5. Hosking, J. S., A. Orr, G. J. Marshall, J. Turner, and T. Phillips (2013), The influence of the Amundsen-Bellingshausen Seas Low on the climate of West Antarctica and its representation in coupled climate model simulations, J. Clim., 26, 6633–6648, doi:10
  6. McMillan, M., A. Shepherd, A. Sundal, K. Briggs, A. Muir, A. Ridout, A. Hogg, and D. Wingham (2015), Increased ice losses from Antarctica detect ed by CryoSat-2, Geophys. Res. Lett., 41, 3899– 3905, doi:10.1002/2014GL060111.
  7. Thomas, E. R., J. S. Hosking, R. R. Tuckwell, R. A. Warren, and E. C. Ludlow (2015), Twentieth century increase in snowfall in coastal West Antarctica, Geophys. Res. Lett., 42, 9387–9393, doi:10.1002/2015GL065750.
  8. Raphael, M.N., G.J. Marshall, J. Turner, R. Fogt, D.P. Schneider, D.A. Dixon, J.S. Hosking, J. Jones, and W. Hobbs, 2015: The Amundsen Sea Low: Variability, change and impact on Antarctic climate. Bull. Am. Met. Soc.

Key Figures

Click the thumbnails to view larger sizes

Thumbnails

Captions
An example of seasonal mean sea level pressure around Antarctica with the location of the ASL marked with a '+' symbol. The sector used to derive the ASL indices (version 2) is enclosed by the black line box.(contributed by S. Hosking)
Time series of monthly mean ASL longitudinal location derived from ERA- Interim data (grey line) and the corresponding 11-month smoothed time series (black line). (contributed by S. Hosking)

Cite this page

Hosking, Scott & National Center for Atmospheric Research Staff (Eds). Last modified 14 Jan 2020. "The Climate Data Guide: Amundsen Sea Low indices ." Retrieved from https://climatedataguide.ucar.edu/climate-data/amundsen-sea-low-indices.

Acknowledgement of any material taken from this page is appreciated. On behalf of experts who have contributed data, advice, and/or figures, please cite their work as well.

Amundsen Sea Low indices

The Amundsen Sea Low (ASL) is a climatological low pressure center located over the extreme southern Pacific Ocean, off the coast of West Antarctica.  Atmospheric variability in this region is larger than anywhere else in the Southern Hemisphere, and exhibits significant correlations with both the Southern Annular Mode (SAM) and ENSO.  Given its linkages to basin-wide ENSO variability, the ASL may be thought of as a Southern Hemisphere analog to the Aleutian Low (see North Pacific Index).  The ASL plays a significant role in the climate variability of West Antarctica and the adjacent oceanic environment.  Due to the extreme variability in the ASL region, and the seasonal migration of the ASL's low-pressure center, defining a single index of the ASL is challenging.  A consistent set of indices of the ASL, including its absolute and relative central pressure, and the latitude and longitude of these central pressures, has been derived from the ECMWF reanalysis.  The term Amundsen-Bellingshausen Seas Low (ABSL) is another name for the ASL.

1979-01/2020-01

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