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首页> 外文期刊>Advances in Meteorology >A Comparison of Southern Hemisphere Cyclone Track Climatology and Interannual Variability in Coarse-Gridded Reanalysis Datasets
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A Comparison of Southern Hemisphere Cyclone Track Climatology and Interannual Variability in Coarse-Gridded Reanalysis Datasets

机译:粗网格再分析数据集中南半球气旋路径气候和年际变化的比较

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摘要

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 Ni?o 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.
机译:南半球(SH)温带气旋的研究少于北半球(NH)。由于数据的可靠性,尤其是在1979年之前,从全球再分析数据集中生成SH气旋径迹是有问题的。因此,比较来自不同再分析数据集的SH气旋径迹的气候和变化是谨慎的。我们从三个再分析数据集中生成了气旋的跟踪频率和强度气候:国家环境预测中心的再分析I和再分析II数据集以及欧洲中型天气预报中心ERA-40数据集。我们的结果表明,与NCEP再分析相比,ERA-40在SH活跃旋风区域产生更强的旋风。在1979年以后的NCEP重新分析数据中,在SH活跃旋风区域还发现了更强烈的风暴,这反映了过去几十年AAO的积极趋势。在评估年际变化时,我们的结果显示,包括罗斯南波列车在内的太平洋南美洲(PSA)和东印度洋模式分别响应与厄尔尼诺和印度洋偶极子(IOD)相关的异常加热。对AAO的响应显示出气旋跟踪频率的稳固环形结构,但强度没有显示旋风频率与气旋强度之间的弱关系。

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