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of 45˚N. This subset comprised 2016 observations <strong>from</strong> 165 storms during 1988 – 2006. Several tests<br />

are done to statistically justify the design of the algorithm using n-fold cross-validation. The resulting<br />

averaged mean absolute error is 10.9 kt (50% of points are within 10 kt) or 8.4 mb (50% of points are<br />

within 8 mb); its accuracy is on par with other objective techniques.<br />

3 Conclusion and Future work<br />

Further improvements of FASI are also possible. Given the global coverage of HURSAT, it is possible<br />

that a training set could be constructed for the Western North Pacific during the period of aircraft<br />

reconnaissance (1980-1987). Such an approach would be unique to FASI since other objective<br />

algorithms mentioned here have been developed over the North Atlantic. This approach will also allow a<br />

climatological application: a global estimate of TC activity based on FASI that could be validated in two<br />

separate basins.<br />

Temporal constraints on changes in intensity could also be applied to the algorithm in the future.<br />

The FASI algorithm has no dependency upon time except that which is implied by the use of features<br />

<strong>from</strong> previous satellite images (6, 12, and 24 hours prior). Other objective algorithms use temporal<br />

constraints on intensity changes (e.g., the ADT and Subjective DT). Including similar constraints in FASI<br />

would likely decrease some of the random error reported herein.<br />

Another application of the FASI technique would be to include it in a satellite consensus<br />

(SatCon) technique, which incorporates strengths and weaknesses of several objective estimates to<br />

compute an intensity estimate that is better than the any of its individual parts [6]. The FASI technique<br />

may well provide independent information for such an approach.<br />

Finally, the FASI technique can be combined with an algorithm to detect the TC center of<br />

circulation for full automation of the technique. But again, this would require some further analysis of the<br />

center location algorithms performance using HURSAT data.<br />

In short, the FASI technique provides a unique approach to estimate the intensity of tropical<br />

cyclones. The error statistics of the technique are on par with other algorithms. This approach has the<br />

potential to provide global TC intensity estimates that could augment intensity estimates made by other<br />

objective techniques.<br />

Acknowledgements This work was supported by the Expeditions in Computing Program of the<br />

National Science Foundation under award CCF-1029731. Special thanks are given to Jim Kossin and<br />

Carl Schreck who provided valuable insight during the development of this work. The opinions<br />

expressed in this paper are those of the authors. They do not necessarily reflect the official views or<br />

policies of NSF, NOAA, Department of Commerce, or the US Government.<br />

References<br />

[1] C. S. Velden and coauthors. The Dvorak tropical cyclone intensity estimation technique: A satellitebased<br />

method that has endured for over 30 years. Bull. Amer. Meteor. Soc., 87, 1195 – 1210, 2006.<br />

[2] E. A. Ritchie, G. Valliere-Kelley, M. F. Piñeros, and J. S. Tyo. <strong>Tropical</strong> cyclone intensity estimation<br />

in the North Atlantic Basin using an improved deviation angle variance technique. Weather and<br />

Forecasting, 27, 1264-1277, 2012.<br />

[3] G. Fetanat, A. Homaifar and K. Knapp. <strong>Objective</strong> <strong>Tropical</strong> <strong>Cyclone</strong> <strong>Intensity</strong> <strong>Estimation</strong> using<br />

Analogs of Spatial Features in <strong>Satellite</strong> Data. Weather and Forecasting, 2013 (Accepted).<br />

[4] G. Fetanat, A. Homaifar and K. Knapp. <strong>Tropical</strong> <strong>Cyclone</strong> <strong>Intensity</strong> <strong>Estimation</strong> using Spatial Features<br />

in <strong>Satellite</strong> Data and Temporal Analysis. 30th AMS Conference On Hurricanes and <strong>Tropical</strong><br />

Meteorology, 2012.<br />

[5] K. R. Knapp and J. P. Kossin. New global tropical cyclone data <strong>from</strong> ISCCP B1 geostationary<br />

satellite observation. Journal of Applied Remote Sensing, 1, 013505, 2007.<br />

[6] D. Herndon and C. Velden. CIMSS TC intensity satellite consensus (SATCON). 62nd<br />

Interdepartmental Hurricane Conference, Charleston, SC., 2008.

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