Abstract

Thirty-year (1980–2009) tropical cyclone (TC) images from geostationary satellite (GOES, Meteosat, GMS, MTSAT and FY2) infrared sensors covering the Northwestern Pacific were used to build a TC size dataset based on objective models. The models are based on a correlation between the size of TCs, defined as the mean azimuth radius of 34 kt surface winds (R34) and the brightness temperature radial profiles derived from satellite imagery. Using satellite images between 2001 and 2009, we obtained 16,548 matchup samples and found the correlation to be positive in the TC’s inner core region (in the annulus field 64 km from the TC center) and negative in its outer region (in the annulus field 100–250 km from the TC center). Then, we performed a stepwise regression to select the dominant variables and derived the associated coefficients for the objective models. Independent validation against best track archives shows the median estimation error to be between 27 and 65 km, which are not significantly different to other satellite series data. Finally, we applied the models to 721 TCs and made 13,726 measurements of TC size. The difference of mean TC size derived from our models, and also that from the US Joint Typhoon Warning Center (JTWC) best track archives is 19 km. The developed database is valuable in the research fields of TC structure, climatology, and the initialization of forecasting models.

Highlights

  • The Northwest Pacific (NWP) is a region where tropical cyclones (TCs) generate very frequently [1].TCs are severe storms formed over tropical waters, and they are characterized by a non-frontal synoptic-scale low-pressure weather system, with organized convection and clearly-defined cyclonic surface wind circulation [1,2]

  • The results showed that fast-moving, strong or recurving TCs have a larger size than slow-moving, weak, or non-recurving TCs

  • The use of high temporal and spatial resolution geostationary satellite infrared observations to construct a set of TC size climatological datasets is feasible and valuable in research on changes in TC structure, climatology, and the initialization and improvement of numerical forecasting models [36]

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Summary

Introduction

The Northwest Pacific (NWP) is a region where tropical cyclones (TCs) generate very frequently [1]. Storm-centered infrared imagery of TCs and an 850 hPa mean tangential wind (from model analyses) at a radius of 500 km, and formed a global TC size climatology. Using this definition, Knaff et al [6]. The use of high temporal and spatial resolution geostationary satellite infrared observations to construct a set of TC size climatological datasets is feasible and valuable in research on changes in TC structure, climatology, and the initialization and improvement of numerical forecasting models [36].

Datasets
TC Size Dataset Derived from Satellite Observations in the NWP
Result with Different
TC Size Dataset in the NWP Covering 1980 and 2009
TC Size Climatology
Correlation between TC Size and Intensity
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Findings
Summary
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