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Mechanism of Asymmetric Precipitation by Tropical Cyclone Nada Over the Indian Peninsula Cover

Mechanism of Asymmetric Precipitation by Tropical Cyclone Nada Over the Indian Peninsula

Open Access
|Apr 2022

Figures & Tables

Table 1

Position, time, intensity, and MSLP (MSW: maximum sustained wind speed; and MSLP: minimum sea-level pressure).

LAT. (°N)LON. (°E)TIMEMSW (M·S–1)MSLP (MB)
7.287.911/29/1215.41000
7.886.911/29/1818996
8.586.011/30/0020.6993
9.484.711/30/0623989
9.883.811/30/1223989
10.282.911/30/1823989
10.382.112/01/0020.6993
10.481.312/01/0620.6993
10.880.512/01/1218996
10.880.112/01/1812.81004
10.979.612/02/0010.31007
1178.912/02/0610.31007
Figure 1

Track (a) and intensity (b) of TC Nada. The locations of the TC center every 6 hours are represented by black circles in the time format of year-month-day-hour, the two dashed black lines indicate 10.5°N and 82.2°E, respectively, and the solid box A indicates the study box (8°N–12°N, 77°E–81°E) in (a). The solid black line and the dashed line indicate the minimum sea-level pressure and maximum sustained wind speed of the TC in (b), respectively.

Figure 2

Daily precipitation distribution during the passage of Nada (the color bar represents rainfall (in mm)).

Figure 3

Time series of the maximum wind speed radius (polyline, unit in km) and average precipitation rate in Box A (bar, unit in mm/hr) during the track of Nada.

Figure 4

Wind field (vanes) and water vapor flux (shaded; in g/(cm·hPa·s)) at 850 hPa (a–c) and 300 hPa (d–f) on December 1.

Figure 5

Water vapor flux divergence (shaded; unit in × 10–8 g/(cm2·hPa·s) at 850 hPa (a–c) and 300 hPa (d–f) on December 1.

Figure 6

The air temperature ((shaded; unit in°C)) at 850 hPa during the passage of Nada.

Figure 7

Vertical and horizontal cross-sections of air temperature (contour; unit in°C) along 82.2°E (a) and 10.5°N (b) at 06:00 UTC on December 1.

Figure 8

Vertical velocity (contour; unit in pa/s) along latitude 10.4°N (a) and longitude of 81.3°E (b) at the TC center at 06:00 UTC on December 1.

Table 2

Corresponding height of the maximum vertical velocity along with the longitudinal and zonal distribution near the TC center at 06:00 UTC on December 1.

ZONALLONGITUDINAL
MAXIMUM (PA/S)HEIGHT (HPA)MAXIMUM (PA/S)HEIGHT (HPA)
Upward movement0.91000–5000.71000–650
Subsidence motion0.2500–3000.2600–300
Figure 9

Water vapor flux (contour; in g/(cm·hPa·s)) along latitude 10.4°N (a) and longitude 81.3°E (b) at the TC center at 06:00 UTC on December 1.

Figure 10

The pseudoequivalent potential temperature (contour; unit in K) at the TC center at 06:00 UTC on December 1 along latitude 10.4°N (a) and longitude 81.3°E (b).

Figure 11

Vorticity (contour; unit in × 10–4 s–1) at 850 hPa (a–c) and at 300 hPa (d–i) during the passage of Nada.

Figure 12

Vertical wind shear (shade; unit: m/s) and wind field (vanes; unit: m/s) of the entire convective layer (200–850 hPa).

Figure 13

The mechanism of precipitation induced by TC Nada.

DOI: https://doi.org/10.16993/tellusa.32 | Journal eISSN: 3035-9554
Language: English
Page range: 159 - 171
Submitted on: Feb 17, 2022
Accepted on: Feb 17, 2022
Published on: Apr 5, 2022
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services

© 2022 Haibin Lü, Xueting Xing, Honghua Zhang, Yusheng Cui, Chu qi Xia, Simei Tan, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.