Mapping the Antarctic Polar Front: Weekly realizations from 2002 to 2014

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Abstract

We map the weekly position of the Antarctic Polar Front (PF) in the Southern Ocean over a 12-year period (2002-2014) using satellite sea surface temperature (SST) estimated from cloud-penetrating microwave radiometers. Our study advances previous efforts to map the PF using hydrographic and satellite data and provides a unique realization of the PF at weekly resolution across all longitudes (doi:10.1594/PANGAEA.855640). The mean path of the PF is asymmetric; its latitudinal position spans from 44 to 64° S along its circumpolar path. SST at the PF ranges from 0.6 to 6.9 °C, reflecting the large spread in latitudinal position. The average intensity of the front is 1.7 °C per 100 km, with intensity ranging from 1.4 to 2.3 °C per 100 km. Front intensity is significantly correlated with the depth of bottom topography, suggesting that the front intensifies over shallow bathymetry. Realizations of the PF are consistent with the corresponding surface expressions of the PF estimated using expendable bathythermograph data in the Drake Passage and Australian and African sectors. The climatological mean position of the PF is similar, though not identical, to previously published estimates. As the PF is a key indicator of physical circulation, surface nutrient concentration, and biogeography in the Southern Ocean, future studies of physical and biogeochemical oceanography in this region will benefit from the provided data set.

Figures

  • Figure 1. Example of (a) spatial and (b) thermal discontinuity resulting in an adjustment in the PF location according to Eq. (1) as outlined in Sect. 2.2.2. dl, 2σl in units of ◦latitude and dt , 2σt in units of ◦C.
  • Figure 2. Example cases when spatial and thermal discontinuity is justified: frontal filaments (a) disconnected or (b) situated northsouth.
  • Table 1. Estimated PF location RMS error (degrees of latitude) and sample size (n), by sector.
  • Figure 3. PF location identified from surface XBT data (timestamp indicated) overlain on the corresponding weekly satellite-estimated 1SST and PF realization in the (a) Australian, (b) Drake Passage, and (c) African sectors.
  • Figure 4. Southern Ocean (a) mean SST and (b) absolute SST gradient with climatological PF overlain (June 2002–February 2014).
  • Figure 5. Climatological (a) PF location and (b) SST, (c) absolute SST gradient, and (d) bottom depth at the PF (June 2002– February 2014). Statistically significant (> 95 %) correlation coefficients with bottom depth are indicated in the top right corner of (a)–(c).
  • Figure 6. The climatological position of the PF in this and previous studies overlain on bottom topography obtained from the National Geophysical Data Center (www.ngdc.noaa.gov/mgg/dat/ misc/predicted_seafloor_topography/TOPO/), where light (dark) shading indicates shallow (deep) bathymetry.

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CITATION STYLE

APA

Freeman, N. M., & Lovenduski, N. S. (2016). Mapping the Antarctic Polar Front: Weekly realizations from 2002 to 2014. Earth System Science Data, 8(1), 191–198. https://doi.org/10.5194/essd-8-191-2016

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