High-resolution quantitative precipitation forecasts and simulations by the Cloud-Resolving Storm Simulator (CReSS) for Typhoon Morakot (2009)

Chung-Chieh Wang, Hung Chi Kuo, Tien Chiang Yeh, Chao Hsuan Chung, Yu Han Chen, Shin Yi Huang, Yi Wen Wang, Ching Hwang Liu

Research output: Contribution to journalArticle

14 Citations (Scopus)

Abstract

Typhoon Morakot (2009) struck Taiwan during 7-9 August 2009, and brought extreme rainfall up to 2855. mm and the worst damages in the past 50. years. The operational models showed deficiency and serious under-prediction in rainfall amount at real time. This study demonstrates that the Cloud-Resolving Storm Simulator (CReSS), a state-of-the-art, high-resolution model, at a grid size of 3. km and starting as early as 0000 UTC 4 August, can successfully simulate and reproduce the event with high accuracy, including the distribution and timing of heavy rainfall in Taiwan. In the simulation starting at 0000 UTC 6 August, for example, the threat scores for 24-h rainfall for 8 August (with extreme amounts >1450. mm) reach 0.8-0.4 even at thresholds of 100-500. mm. This result is only possible due to small track error and the phase-locking mechanism of the Taiwan topography to heavy rainfall.Furthermore, real-time forecast and hindcast integrations of the CReSS model show that high-quality quantitative precipitation forecasts (QPFs) with peak total amount 67-80% of the true value are also obtained from initial conditions at 0000 UTC 6 August, which is about 2. days prior to the beginning of the heaviest rainfall in southern Taiwan. In these integrations, typhoon track errors in the global model forecasts used as boundary conditions are the major error source that prevent more ideal QPF results before and at 1200 UTC 5 August. When properly configured, it is believed that other similar cloud-resolving models can achieve comparable performance. Thus, the importance of and potential benefits from deterministic high-resolution forecasts is stressed, which may give an extended lead-time when the track error is small. With potentially longer time window for emergency action just prior to extreme rainfall events when it matters the most, such forecasts may ultimately lead to reduced losses in lives and properties.

Original languageEnglish
Pages (from-to)26-41
Number of pages16
JournalJournal of Hydrology
Volume506
DOIs
Publication statusPublished - 2013 Dec 9

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typhoon
simulator
rainfall
simulation
forecast
boundary condition
topography
damage
prediction

Keywords

  • Cloud-resolving model
  • Morakot (2009)
  • Quantitative precipitation forecasts (QPFs)
  • Taiwan
  • Topography
  • Typhoon

ASJC Scopus subject areas

  • Water Science and Technology

Cite this

High-resolution quantitative precipitation forecasts and simulations by the Cloud-Resolving Storm Simulator (CReSS) for Typhoon Morakot (2009). / Wang, Chung-Chieh; Kuo, Hung Chi; Yeh, Tien Chiang; Chung, Chao Hsuan; Chen, Yu Han; Huang, Shin Yi; Wang, Yi Wen; Liu, Ching Hwang.

In: Journal of Hydrology, Vol. 506, 09.12.2013, p. 26-41.

Research output: Contribution to journalArticle

Wang, Chung-Chieh ; Kuo, Hung Chi ; Yeh, Tien Chiang ; Chung, Chao Hsuan ; Chen, Yu Han ; Huang, Shin Yi ; Wang, Yi Wen ; Liu, Ching Hwang. / High-resolution quantitative precipitation forecasts and simulations by the Cloud-Resolving Storm Simulator (CReSS) for Typhoon Morakot (2009). In: Journal of Hydrology. 2013 ; Vol. 506. pp. 26-41.
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abstract = "Typhoon Morakot (2009) struck Taiwan during 7-9 August 2009, and brought extreme rainfall up to 2855. mm and the worst damages in the past 50. years. The operational models showed deficiency and serious under-prediction in rainfall amount at real time. This study demonstrates that the Cloud-Resolving Storm Simulator (CReSS), a state-of-the-art, high-resolution model, at a grid size of 3. km and starting as early as 0000 UTC 4 August, can successfully simulate and reproduce the event with high accuracy, including the distribution and timing of heavy rainfall in Taiwan. In the simulation starting at 0000 UTC 6 August, for example, the threat scores for 24-h rainfall for 8 August (with extreme amounts >1450. mm) reach 0.8-0.4 even at thresholds of 100-500. mm. This result is only possible due to small track error and the phase-locking mechanism of the Taiwan topography to heavy rainfall.Furthermore, real-time forecast and hindcast integrations of the CReSS model show that high-quality quantitative precipitation forecasts (QPFs) with peak total amount 67-80{\%} of the true value are also obtained from initial conditions at 0000 UTC 6 August, which is about 2. days prior to the beginning of the heaviest rainfall in southern Taiwan. In these integrations, typhoon track errors in the global model forecasts used as boundary conditions are the major error source that prevent more ideal QPF results before and at 1200 UTC 5 August. When properly configured, it is believed that other similar cloud-resolving models can achieve comparable performance. Thus, the importance of and potential benefits from deterministic high-resolution forecasts is stressed, which may give an extended lead-time when the track error is small. With potentially longer time window for emergency action just prior to extreme rainfall events when it matters the most, such forecasts may ultimately lead to reduced losses in lives and properties.",
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AB - Typhoon Morakot (2009) struck Taiwan during 7-9 August 2009, and brought extreme rainfall up to 2855. mm and the worst damages in the past 50. years. The operational models showed deficiency and serious under-prediction in rainfall amount at real time. This study demonstrates that the Cloud-Resolving Storm Simulator (CReSS), a state-of-the-art, high-resolution model, at a grid size of 3. km and starting as early as 0000 UTC 4 August, can successfully simulate and reproduce the event with high accuracy, including the distribution and timing of heavy rainfall in Taiwan. In the simulation starting at 0000 UTC 6 August, for example, the threat scores for 24-h rainfall for 8 August (with extreme amounts >1450. mm) reach 0.8-0.4 even at thresholds of 100-500. mm. This result is only possible due to small track error and the phase-locking mechanism of the Taiwan topography to heavy rainfall.Furthermore, real-time forecast and hindcast integrations of the CReSS model show that high-quality quantitative precipitation forecasts (QPFs) with peak total amount 67-80% of the true value are also obtained from initial conditions at 0000 UTC 6 August, which is about 2. days prior to the beginning of the heaviest rainfall in southern Taiwan. In these integrations, typhoon track errors in the global model forecasts used as boundary conditions are the major error source that prevent more ideal QPF results before and at 1200 UTC 5 August. When properly configured, it is believed that other similar cloud-resolving models can achieve comparable performance. Thus, the importance of and potential benefits from deterministic high-resolution forecasts is stressed, which may give an extended lead-time when the track error is small. With potentially longer time window for emergency action just prior to extreme rainfall events when it matters the most, such forecasts may ultimately lead to reduced losses in lives and properties.

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