2011
DOI: 10.1007/s13351-011-0506-9
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A western North Pacific tropical cyclone intensity prediction scheme

Abstract: A western North Pacific tropical cyclone (TC) intensity prediction scheme (WIPS) is developed based on TC samples from 1996 to 2002 using the stepwise regression technique, with the western North Pacific divided into three sub-regions: the region near the coast of East China (ECR), the South China Sea region (SCR), and the far oceanic region (FOR). Only the TCs with maximum sustained surface wind speed greater than 17.2 m s −1 are used in the scheme. Potential predictors include the climatology and persistence… Show more

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Cited by 17 publications
(11 citation statements)
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“…The losses caused by these disasters have also continued to increase in recent years. The western North Pacific (WNP) is one of the oceanic regions most prone to typhoons [3][4][5][6][7][8][9]. Since China is located on the west coast of the WNP, it is greatly affected by typhoons, particularly along the east coast [10].…”
Section: Introductionmentioning
confidence: 99%
“…The losses caused by these disasters have also continued to increase in recent years. The western North Pacific (WNP) is one of the oceanic regions most prone to typhoons [3][4][5][6][7][8][9]. Since China is located on the west coast of the WNP, it is greatly affected by typhoons, particularly along the east coast [10].…”
Section: Introductionmentioning
confidence: 99%
“…The intensification potential (POT) is defined as the difference between MPI and the current intensity. The POT is considered the most important predictor in the statistical-dynamical TC intensity prediction models (Chen et al, 2011;DeMaria & Kaplan, 1994, 1999. In particular, DAT-based POT shows the highest correlation coefficient with intensity change (Kim et al, 2018).…”
Section: Resultsmentioning
confidence: 99%
“…The chief reason for the choice of parameters is that these dynamic and thermodynamic conditions are essential for the strengthening and/or maintaining of storm (Bister and Emanuel, 1998; Hendricks et al ., 2010; Tang and Emanuel, 2010; Chen et al ., 2011; Mei et al ., 2015; Nguyen and Molinari, 2015). Such as the inflow of zonal wind can be characterized as the rapid intensification of storm; the intrusion of cold air from mid‐upper troposphere and the outflow of zonal wind can abate the storm's strength; the interplay between the meso‐scale vortex and the cyclonic vortex has a non‐linear relationship with the storm's strength; sea surface temperature, total vapour flux and specific humidity provide the hydrothermal condition for the development and strengthening of cyclone; The vertical wind shear could destroy the warm core of cyclone in most cases and has inhibition on the storm's strength; the sea level pressure around the storm's centre has a close correlation relationship with the storm's strength;…”
Section: Data Methods and Experimental Designmentioning
confidence: 99%