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The storms of October 2000


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Contents

Introduction
The storms of 28 - 30 October

The passage of a depression - the example of 30 October storm

Exercises

The passage of a depression

The example of the 30 October storm

The changes in weather features which took place in southern England on 30 October, were a typical example of the marked changes that can happen when an intense and well-developed frontal system passes over during the winter months. The table below shows the typical changes that occur in weather features.

Table 1. The typical changes in weather features associated with the passage of a mature depression across the UK in the winter months
  Ahead of the warm front The passage of the warm front The warm sector The passage of the cold front The cold sector
Pressure
starts to fall steadily continues to fall steadies starts to rise continues to rise
Temperature
quite cold, starts to rise continues to rise quite mild sudden drop remains cold
Cloud cover
cloud base drops and thickens (cirrus and altostratus) cloud base is low and thick (nimbostratus) cloud may thin and break clouds thicken (sometimes with large cumulonimbus) clouds thin with some cumulus
Wind speed and direction
speeds increase and direction backs veers and becomes blustery with strong gusts remain steady, backs slightly speeds increase, sometimes to gale force, sharp veer winds are squally
Precipitation
none at first, rain closer to front, sometimes snow on leading edge continues, and sometimes heavy rainfall rain turns to drizzle or stops heavy rain, sometimes with hail, thunder or sleet showers
 
The passage of the warm and cold front can be seen clearly on Figs 5, 6 and 7, which show the synoptic pressure charts for 0000, 0600 and 1200 UTC on 30 October. fig 5
Figure 5. 0000 UTC, 30 October 2000
Figure 6. 0600 UTC, 30 October 2000
fig 6
Figure 7. 1200 UTC, 30 October 2000
fig 7

Table 2 shows the changes in rainfall amounts and temperature that took place every hour at the weather station at Heathrow Airport between 1000 on 29 October and 1700 on 30 October. The changes can be easily linked with the passage of this depression. Temperatures start to rise as the warm front passes over in the early hours of 30 October. They remain high until around 0600, as the warm sector passes over. Further rain occurs as the warm air is undercut by descending cold air from the occlusion. A sharp decrease in temperatures takes place as the cold front approaches around 0700. A heavy period of rain then occurs as this front passes over, before easing off in mid-morning as the cold sector passes over behind the warm front.

Table 2 . Changes in rainfall/temperature, Heathrow Airport, between 1000 on 29 October and 1700 on 30 October
Date
Time
Rainfall amount (mm)
Dry bulb temp (°C)
29/10/00
1000
0.0
10.0
29/10/00
1100
0.0
10.8
29/10/00
1200
0.0
11.6
29/10/00
1300
0.0
11.6
29/10/00
1400
0.0
11.8
29/10/00
1500
0.0
11.6
29/10/00
1600
0.0
10.5
29/10/00
1700
0.2
10.8
29/10/00
1800
1.6
11.4
29/10/00
1900
2.0
12.1
29/10/00
2000
2.4
11.7
29/10/00
2100
2.4
12.7
29/10/00
2200
1.6
13.2
29/10/00
2300
0.8
11.4
30/10/00
0000
5.4
13.1
30/10/00
0100
2.4
13.3
30/10/00
0200
2.4
13.2
30/10/00
0300
1.6
13.1
30/10/00
0400
1.6
13.0
30/10/00
0500
2.0
13.1
30/10/00
0600
1.4
12.8
30/10/00
0700
2.8
9.8
30/10/00
0800
5.0
10.2
30/10/00
0900
1.0
8.9
30/10/00
1000
0.0
8.4
30/10/00
1100
0.0
6.6
30/10/00
1200
0.2
7.6
30/10/00
1300
0.4
9.9
30/10/00
1400
0.2
10.8
30/10/00
1500
0.0
11.3
30/10/00
1600
0.0
11.0
30/10/00
1700
0.0
10.5

next: Exercises

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