This research produces an objective, track-based climatology of Rossby wave packets (RWPs) and tests the sensitivity of the results to changes in the methods used in filtering the raw data and in tracking. NCEP/NCAR Reanalysis wind and geopotential height data at 300 hPa every 6 hours were spectrally filtered using a Hilbert transform technique under the assumption that RWPs propagate along a waveguide defined by the 14-day running average of the 300 hPa wind. After some spatial smoothing, the local maxima in RWP envelope amplitude (WPA) were tracked using two objective techniques: a point-based cost optimization routine and a hybrid of point identification and object-based tracking following rules similar to those used in the tracking of tropical convective clusters. The total energy flux term of the eddy kinetic energy equation was used as a cross-check for the purpose of hand-verifying RWP tracks in order to compare the performance of each tracking method. Track data and object-based descriptive statistics (including area, average intensity, intensity volume, intensity-weighted centroid position and velocity) were gathered to describe the inter-annual, annual, seasonal, and regime-based climatology of RWPs.
When tracking methods are verified over two winter seasons and compared, the hybrid technique statistically outperforms point-based tracking, particularly when estimating track duration and propagation. When long lived RWPs are verified, there is strong evidence that some RWPs can last over 30 days and circumnavigate the Northern (Southern) Hemisphere up to two (three) times. RWPs are found to exhibit a much more pronounced seasonal cycle in the Northern Hemisphere, where they are nearly non-existent in the summer months (JJA), as compared to nearly continuous RWP activity downwind of South Africa during Austral Summer (DJF). Interannual variability in packet frequency and intensity in the Northern Hemisphere is found to be strongly connected with the large scale flow regime, with oscillatory patterns like ENSO and the AO playing significant roles. Enhanced WPA is also found to coherently propagate in composites of regime change events (e.g. a reversal of the AO). No significant long-term changes in RWP frequency or intensity are found; however, the North Pacific storm track appears to have shifted northward in the last thirty years.
|Advisor:||Colle, Brian A.|
|Commitee:||Chang, Edmund K., Hameed, Sultan|
|School:||State University of New York at Stony Brook|
|Department:||Marine and Atmospheric Science|
|School Location:||United States -- New York|
|Source:||MAI 54/04M(E), Masters Abstracts International|
|Keywords:||Atmospheric waves, Climatology, Fluid dynamics, Rossby waves, Synoptic meteorology, Teleconnections|
Copyright in each Dissertation and Thesis is retained by the author. All Rights Reserved
The supplemental file or files you are about to download were provided to ProQuest by the author as part of a
dissertation or thesis. The supplemental files are provided "AS IS" without warranty. ProQuest is not responsible for the
content, format or impact on the supplemental file(s) on our system. in some cases, the file type may be unknown or
may be a .exe file. We recommend caution as you open such files.
Copyright of the original materials contained in the supplemental file is retained by the author and your access to the
supplemental files is subject to the ProQuest Terms and Conditions of use.
Depending on the size of the file(s) you are downloading, the system may take some time to download them. Please be