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Xie , B., and F. Zhang, 2012: Impacts of typhoon

Impacts of typhoon track and island topography on the heavy rainfalls in Taiwan associated with Morakot (2009). Xie , B., and F. Zhang, 2012: Impacts of typhoon track and island topography on the heavy rainfalls in Taiwan associated with Morakot

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Xie , B., and F. Zhang, 2012: Impacts of typhoon

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  1. Impacts of typhoon track and island topography on the heavy rainfalls in Taiwan associated with Morakot (2009) Xie, B., and F. Zhang, 2012: Impacts of typhoon track and island topography on the heavy rainfalls in Taiwan associated with Morakot (2009). Mon. Wea. Rev., 140, 3379–3394.

  2. Outline • Keywords • Introduction • The forecast model • Overview of Morakot and performance of the WRF control and reference simulations • Sensitivity of the rainfall to Morakot’strack • Orographic precipitation enhancement • The monsoon–typhoon interaction • Summary and conclusions • Reference

  3. Keywords • Normalized absolute precipitation error (NAPE) : N- the total number of grid points with precipitation in either the observation and/or the simulation. Ri- the precipitation in an ensemble member. Roi- the precipitation in an observation. A smaller value of NAPE indicates a better forecast of precipitation.

  4. Introduction • Taiwan suffers from heavy rains and flood disasters caused by TCs each year. Because of the complex topographic features and their interactions with TCs, it is extremely hard to predict the track, intensity change, and precipitation of TCs as they approach land .(Yeh and Elsberry 1993;Wu and Kuo 1999;Wu 2001; Jian andWu 2008) • The southwesterly monsoon flow is believed to be responsible for supplying large amounts of moisture to the TC environments during the monsoon season (e.g., Chiao and Lin 2003; Wu et al. 2009; Ge et al. 2010; Hong et al. 2010; Wu et al. 2011; Liang et al. 2011; Nguyen and Chen 2011; Chien and Kuo 2011). • However, monsoon plays in the heavy rainfall is difficult to elucidate since the monsoon is a large-scale system, acting as a background environment.

  5. Zhang et al. 2010 (Z10) examined the predictability of Morakot with a cloud-resolving ensemble initialized with analysis andflow-dependent perturbations obtained from a real time global ensemble data assimilation (EDA) system. And they were able to predict this record-breaking rainfall event. • Fang et al. [2011 (F11)] found that the orography is crucial in determining the structure, intensity, and variability of Morakot’s rainfall. • Both of Z10 and F11 concluded that the forecasting of extreme rainfall events such as Morakot would benefit from probabilistic prediction provided by a high-resolution mesoscale ensemble forecast system.

  6. The primary focuses of the current study are 1) the relationship between predictability of the typhoon track and precipitation. 2) the enhancement of orographically induced rainfall. 3) the interactions between the southwest monsoon and Morakot.

  7. The forecast model • WRF(Skamarock et al. 2007) • - 2 two-way-nested model domains. • - Initiation: • a) 0000 UTC 5 Aug. (CNTL00) • b) from Global EDA system[Z10] • Global EDA system: • - 60 members (flow-dependence uncertainty) • - Period: 0000 UTC 5 Aug. • ~ 1200 UTC 10 Aug. (132h) • - No cumulus parameterization. • - Microphysics scheme: the WRF • Single-Moment 6-class(WSM6) graupel. • Observed track and intensity • data : JTWC • The Final Operation Global • (FNL) analysis data: NCEP • (for synoptic analysis and comparison.) d01

  8. Overview of Morakot and performance of the WRF control and reference simulations • Despite only having the intensity of a category-2 storm, Morakot brought record-breaking rainfall with 2777 mm in 72 h (Z10). • 2 August 2009(tropical depression)  5 August (T.C) 7 August (945hPa)(before landfall)  11 August (Aparted to China) • The strongest rainfall occurred between 0000 UTC 8 August and 0000 UTC 9 August (Z10; Hong et al. 2010; F11).

  9. H H Strong updraft 850-hPa wind (full wind barb is 10 m /s) 850-hPa Geopotential height (solid contour lines; from 1150 to1530 m by every 40 m) 500-hPa height (dashed contour lines; from 5440 to 5880 m by every 40 m) Precipitable water (PW,shaded; kg /m^2)

  10. Sensitivity of the rainfall to Morakot’strack a) Ensemble-based analysis -The members with good track forecasts also produced good rainfall forecasts. [Z10] Track error: distance between the positions of the ensemble member and best-track observations. (averaged from the 3-h a prior and posterior to landfall time.) NAPE: 72-h accumulated precipitation error. (from 0000UTC6 Aug to 0000UTC9 Aug) 95% confidence level The accuracy of the quantitative precipitation forecast (QPF) for Morakotis closely related to the predictability of its track.

  11. Missed landfall Error< 25km Good performance. Forecast from ensemble mean. Best performance. The 72-h accumulated rainfall (shaded; mm) of Typhoon Morakot over Taiwan(from 0000UTC6 Aug to 0000UTC9 Aug)

  12. b) Sensitivity experiment of moved terrain - CNTL00 (good QPF)  MOVE00 - CNTL54 (poor QPF)  MOVE54 SST and atmosphere are extrapolated from nearby. v 160km 200km Moved terrain. This again highlights the importance of track forecast accuracy, as well as Taiwan’s topography, to the accuracy of the QPF.

  13. Orographic precipitation enhancement a. No-terrain experiments - OCEAN CNTL00*45% Morakot brings extremely heavy and asymmetrically distributed rainfall to Taiwan Island even if there is no topography or land. (Same as F11.) The 72-h accumulated rainfall (shaded; mm) of Typhoon Morakot over Taiwan(from 0000UTC6 Aug to 0000UTC9 Aug)

  14. the vertical wind shear can influence the storm motion and the distribution of associated convection (Corbosiero and Molinari 2002, 2003;Cecil 2007; Gao et al. 2009). • The rainfallmay also appear more substantial on the downshear left if the falling hydrometers in this sector are advected by the TC’s cyclonic circulation (e.g., Frank and Ritchie 1999).

  15. vector; m/(s*hPa) The vertical wind shear between 200 and 700 hPa, shaded; mm 3-h accumulated rainfall

  16. a. No-terrain experiments - LAND It is primarily the island topography, not the land interaction that causes the redistribution of the rainfall.

  17. in the inner domain over Taiwan maximum rainfall the presence of Taiwan Island leads to the redistribution of rainfall over elevated terrain, but does not necessarily extract more water from the atmosphere. The 72-h accumulated rainfall (shaded; mm) of Typhoon Morakot over Taiwan(from 0000UTC6 Aug to 0000UTC9 Aug)

  18. in the inner domain over Taiwan maximum rainfall Full terrain * 70% 30% 2247,64% b. Sensitivity to terrain height - HALF 1410,49% 10% 1067,58% 1341,72% 3% the impact of the topography by no means has a linear relationship to the terrain heights or terrain slopes, even if the rainfall is only averaged over the island where the terrain heights are changed. The 72-h accumulated rainfall (shaded; mm) of Typhoon Morakot over Taiwan(from 0000UTC6 Aug to 0000UTC9 Aug)

  19. The meridional mean of the 72-h accumulated rainfall distribution averaged over the heavy rainfall region in Taiwan Island CNTL15 CNTL00 CNTL23

  20. the meridional mean of the 72-h accumulated rainfall distribution averaged over the heavy rainfall region in Taiwan Island HALF-LAND CNTL-HALF HALF-LAND LAND-OCEAN CNTL23 CNTL15 CNTL00

  21. Scatterplots of 72-h accumulated gridpoint rainfall over Taiwan. CNTL-HALF vs. CNTL HALF-LAND vs. HALF LAND-OCEAN vs. LAND windward leeward

  22. The monsoon–typhoon interaction • The southwest monsoon is a large-scale system that is believed to have significant impacts on the development of tropical cyclones in the northwest PacificOcean (Carr and Elsberry 1995; Briegeland Frank 1997; Chen et al. 2004; Wu et al. 2011). • Lee et al. (2011) and Chien and Kuo (2011) highlighted the convergence of the typhoon circulation with the monsoon flow as an important factor for creating a quasi-stationary zonal convective band, which induced the heavy rainfall over Taiwan. • Nguyen and Chen (2011) documented that the combined circulations associated with the tropical storms and monsoon gyre brought in moisture-laden flows toward the western slopes of southern Taiwan that result in heavy rainfall.

  23. Mean 850-hPa wind speed of 96-h forecast in the rectangular region shown in (a) The track and the strength of the typhoon during the first 72 h of the forecast are mostly controlled by the initial conditions of the typhoon circulation within the 600-km radius rather than by the broader environment. The strength of the southwesterly monsoon flow can be strongly enhanced by the approaching typhoon circulation, which leads to stronger convergence and moisture transport. The typhoon circulation at this time is also noticeably stronger and more to the south (closer to the monsoon flow). The 850-hPa wind (full wind barb = 10 m/s) and height (contour from 1340 to 1460 m by every 20 m at 0000 UTC 8 Aug..)

  24. Summary and conclusions • a good rainfall forecast foremost requires a good track forecast during Morakot’s landfall. • The rainfall forecast will be greatly degraded if the island is moved away from the typhoon’s path (MOVE00 versus CNTL00) while the forecast will improve immensely if the island is relocated to the direct path of the storm (MOVE54 versus CNTL54).

  25. The impacts of the island topography on rainfall intensity and distribution were then examined through a series of sensitivity experiments that differ from the three reference simulations (CNTL00, CNTL15, and CNTL23) by reducing all the island terrain heights by half (the HALF experiments), to flat land at sea level (the LAND experiments), or by removing the land and replacing it with ocean (the OCEAN experiments).These sensitivity experiments show that (i) The presence of Taiwan leads to the redistribution of rainfall from the ocean to the island but does not necessarily extract more total water from the atmosphere. (ii) It is primarily the island topography, not the land interaction, that causes the redistribution of the rainfall. (iii) The impact of the topography is by no means a linear function of terrain height or terrain slope.

  26. The strength of the southwesterly monsoon gyre could be strongly enhanced by the approaching typhoon circulation, which leads to stronger convergence and moisture transport near Taiwan. These sensitivity experiments show that the interaction between the typhoon and topography, rather than the location of the monsoon flow, contribute the most to the heavy rainfall caused by Morakot.

  27. Reference • Xie, B., and F. Zhang, 2012: Impacts of typhoon track and island topography on the heavy rainfalls in Taiwan associated with Morakot(2009). Mon. Wea. Rev., 140, 3379–3394. • Zhang, F., Y. Weng, Y.-H. Kuo, J. S. Whitaker, and B. Xie, 2010: Predicting Typhoon Morakot’s catastrophic rainfall with a convection-permitting mesoscale ensemble system. Wea. Forecasting, 25, 1816–1825. • Fang, X., Y.-H. Kuo, and A. Wang, 2011: The impact of Taiwan topography on the predictability of Typhoon Morakot’s record-breaking rainfall: A high-resolution ensemble simulation. Wea. Forecasting, 26, 613–633. • Braun, S. A., and L. Wu, 2007: A numerical study of Hurricane Erin (2001). Part II: Shear and the organization of eyewall vertical motion. Mon. Wea. Rev., 135, 1179–1194. • Meteorological WindowWebsite

  28. Thank you for your attention!!

  29. low-level divergence PV meso-vortex NV meso-vortex low-level convergence Strong storm-relative flow associated with the environmental shear Wu, L., S. A. Braun, J. Halverson, and G. Heymsfield, 2007: A Numerical Study of Hurricane Erin (2001).Part II: Shear and the Organization of Eyewall Vertical Motion.Mon.Wea.Rev. 135, 1179–1194. Figure12.b

  30. 香港、日本、台灣使用十分鐘平均風速值；中國使用兩分鐘平均風速值；聯合颱風警報中心及美國國家颶風中心使用一分鐘平均風速值。 (圖自: 台灣颱風資訊中心)

  31. Precipitable Water (PW,可降水(汽)) 任何兩特定面間，在單位截面積垂直大氣柱內所含全部之水汽， 通常假設全部凝結並收集在同樣單位截面之容器內水應有之高度。 g- 重力 p1 - 空氣柱底部氣壓 p2 - 空氣柱頂部氣壓 X(p) - 氣壓p面上的混合比

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