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The Genesis of Typhoon Nuri as Observed During the Tropical Cyclone Structure 2008 (Tcs-08) Field Experiment – Part 1: the Role of the Easterly Wave Critical Layer : Volume 9, Issue 5 (16/09/2009)

By Montgomery, M. T.

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Book Id: WPLBN0003972870
Format Type: PDF Article :
File Size: Pages 45
Reproduction Date: 2015

Title: The Genesis of Typhoon Nuri as Observed During the Tropical Cyclone Structure 2008 (Tcs-08) Field Experiment – Part 1: the Role of the Easterly Wave Critical Layer : Volume 9, Issue 5 (16/09/2009)  
Author: Montgomery, M. T.
Volume: Vol. 9, Issue 5
Language: English
Subject: Science, Atmospheric, Chemistry
Collections: Periodicals: Journal and Magazine Collection, Copernicus GmbH
Publication Date:
Publisher: Copernicus Gmbh, Göttingen, Germany
Member Page: Copernicus Publications


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Wang, Z., Lussier Iii, L. L., Moore, R. W., & Montgomery, M. T. (2009). The Genesis of Typhoon Nuri as Observed During the Tropical Cyclone Structure 2008 (Tcs-08) Field Experiment – Part 1: the Role of the Easterly Wave Critical Layer : Volume 9, Issue 5 (16/09/2009). Retrieved from

Description: Naval Postgraduate School, Monterey, California, USA. An observational and real-time model forecast study of the genesis of Typhoon Nuri during the Tropical Cyclone Structure 2008 (TCS-08) field campaign in the western North Pacific sector is presented. Analysis and observational data show that the surrounding base state flow was an easterly trade wind flow and the precursor disturbance to Typhoon Nuri was an easterly wave that originated in the ITCZ in the Central Pacific and can be tracked more than 10 days prior to tropical storm formation. An overview of the field data is presented here using a newly proposed dynamical framework for tropical cyclone formation within the critical layer of an easterly wave. Despite propagating through a hostile environment ripe with strong vertical wind shear and relatively dry air, the easterly wave critical layer protected the proto-vortex and allowed it to gestate until it reached a more favorable environment. Within this protective Kelvin's cat's eye flow located within the wave's critical layer existed a sweet spot, defined as the intersection between the wave trough and critical latitude, which was the preferred location for tropical cyclogenesis. Global Forecast System Final Analyses and IR satellite imagery, which shows convective bands wrapping around the sweet spot as genesis nears, confirm that this sweet spot is the location where Typhoon Nuri's dominant low-level circulation emerges.

United States Air Force C130 and Naval Research Laboratory P3 research flights on 16 and 17 August collected flight-level, dropwindsonde, and Doppler radar data that allowed an evaluation of the dynamic and thermodynamic processes within the cat's eye. The dropwindsonde analyses identified the precursor easterly wave disturbance on 16 August and identified an area of weak low-level cyclonic circulation on 17 August.

During the TCS-08 experiment real-time forecasts were produced in real-time using operational global prediction model data to support scientific missions. These forecasts were found to be useful in flight planning discussions and predicted Nuri's genesis latitude within 1.5° 72 h in advance.

The genesis of Typhoon Nuri as observed during the Tropical Cyclone Structure 2008 (TCS-08) field experiment – Part 1: The role of the easterly wave critical layer

Carr III, L. E. and Elsberry, R. L.: Monsoonal interactions leading to sudden tropical cyclone track changes, Mon. Weather Rev., 123, 265–290, 1995.; Chang, C. P., Morris, V. F., and Wallace, J. M.: A statistical study of easterly waves in the western Pacific: July–December 1964. J. Atmos. Sci., 27, 195–201, 1970.; Chen, T. C., Wang, S. Y., Yen, M. C., and Clark, A. J.: Are tropical cyclones less effectively formed by easterly waves in the western North Pacific than in the North Atlantic? Mon. Weather Rev., 136, 4527–4540, 2008.; Deleon, R. P.: The role of subtropical intrusion in the development of Typhoon Usagi (5W) 2007, MS Thesis, Naval Postgraduate School, Monterey, CA, 118 pp, 2008.; Dickinson, M. and Molinari, J.: Mixed Rossby–gravity waves and western Pacific tropical cyclogenesis, Part I: Synoptic evolution, J. Atmos. Sci., 59, 2183–2196, 2002.; Dunkerton, T. J., Montgomery, M. T., and Wang, Z.: Tropical cyclogenesis in a tropical wave critical layer: easterly waves, Atmos. Chem. Phys., 9, 5587–5646, 2009.; Ferreira, R. N. and Schubert, W. H.: Barotropic aspects of ITCZ breakdown, J. Atmos. Sci., 54, 261–285, 1997.; Elsberry, R. L. and Harr, P. A.: Tropical Cyclone Structure (TCS08) field experiment science Basis, observational platforms, and strategy, Asia-Pac. J. Atmos. Sci., 44, 209–231, 2008.; Frank, N. L.: Atlantic tropical systems of 1969, Mon. Weather Rev., 98, 307–314, 1970.; Glickman, T. S.: Glossary of meteorology, American Meteorological Society Boston, USA, 850 pp, 2000.; Gray, W. M.: Global view of the origin of tropical disturbances and storms, Mon. Weather Rev., 96, 669–700, 1968.; Gray, W. M.: Tropical cyclone genesis, Department of Atmos. Sci. Paper No. 323, Colorado State University, Fort Collins, CO, 121 pp, 1975.; Harr, P. A., Elsberry, R. L., and Chan, J. C. L.: Transformation of a large monsoon depression to a tropical storm during TCM-93, Mon. Weather Rev., 124, 2625–2643, 1996.; Hendricks, E. A., Montgomery, M. T., and Davis, C. A.: The role of vortical hot towers in the formation of tropical cyclone Diana (1984), J. Atmos. Sci., 61, 1209–1232, 2004.; Holland, G.: Scale interaction in the western Pacific monsoon, Meteorol. Atmos. Phys., 56, 57–79, 1995.; Lander, M. A.: Description of a monsoon gyre and its effects on the tropical cyclones in the western North Pacific during August 1991, Weather Forecast., 9, 640–654, 1994.; Leipper, D. and Volgenau, D.: Hurricane heat potential of the Gulf of Mexico, J. Phys. Oceanogr., 2, 218–224, 1972.; Molinari, J.: Paradigms of tropical cyclogenesis, B. Am. Meteorol. Soc., 85, 662–663, 2004.; Montgomery, M. T. and Enagonio, J.: Tropical cyclogenesis via convectively forced vortex Rossby waves in a three-dimensional quasigeostrophic model, J. Atmos. Sci., 55, 3176–3207, 1998.; Montgomery, M. T., Nicholls, M. E., Cram, T. A., and Saunders, A. B.: A vortical hot tower route to tropical cyclogenesis, J. Atmos. Sci., 63, 355–386, 2006.; Montgomery, M. T., Wang, Z., and Dunkerton, T. J.: Intermediate and high resolution numerical simulations of the transition of a tropical wave critical layer to a tropical depressi


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