Abstract

Southern Hemisphere (SH) extratropical cyclones have received less study than their Northern Hemisphere (NH) counterparts. Generating SH cyclone tracks from global reanalysis datasets is problematic due to data reliability, especially prior to 1979. It is therefore prudent to compare the climatology and variability of SH cyclone tracks from different reanalysis datasets. We generate cyclone track frequency and intensity climatologies from three reanalysis datasets: The National Center for Environmental Prediction’s Reanalysis I and Reanalysis II datasets and the European Centre for Medium Range Weather Forecasts ERA-40 dataset. Our results show that ERA-40 produces more intense cyclones in the SH active cyclone region compared to NCEP reanalyses. More intense storms are also found in the SH active cyclone region in NCEP reanalyses data post-1979 reflecting the positive trend in the AAO in the past few decades. When evaluating interannual variability, our results show Rossby wave trains including the Pacific South American (PSA) and the East Indian Ocean pattern in response to anomalous heating linked to El Niño and the Indian Ocean Dipole (IOD), respectively. Response to the AAO shows a robust annular structure for cyclone track frequency, but not intensity suggesting a weak relationship between cyclone frequency and cyclone intensity.

Highlights

  • Extratropical cyclones are an important manifestation of the Southern Hemisphere (SH) general circulation and are associated with serious socioeconomic impacts

  • We extend the climatology developed from National Center for Environmental Prediction (NCEP) reanalysis I data by Eichler and Higgins [46] through the year 2010 (NCEP1 5010)

  • 1 2 3 4 5 6 7 8 9 10 (e) between datasets, NCEP2 7910 and NCEP1 7910 showed excellent agreement in their cyclone track frequency and intensity climatologies, which is not surprising given that this comparison was for an updated version of the same reanalysis dataset over the same temporal period

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Summary

Introduction

Extratropical cyclones are an important manifestation of the Southern Hemisphere (SH) general circulation and are associated with serious socioeconomic impacts. We utilized 6 hourly sea-level pressure (SLP) data from 1950 through 2010, with a spatial resolution of 2.5∘× 2.5∘ (lat/lon). Storm tracks were generated from NCEP’s reanalysis II data from 6 hourly sea-level pressure (SLP) data for 1979 through 2010, with a spatial resolution of 2.5∘× 2.5∘ (lat/lon). Similar to NCEP reanalyses I and II datasets, we generated storm tracks from ERA-40 data, and we generated storm tracks from 6 hourly sea-level pressure (SLP) data with a spatial resolution of 2.5∘× 2.5∘ (lat/lon). The time period we chose for our ERA-40 climatology was from 1958 to 2001

Methods
Climatology
Interannual Variability
Findings
Conclusions
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