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Bay City Independent School District Natural Disasters and Weather Extremes

 
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The chance of earthquake damage in Bay City Independent School District is about the same as Texas average and is much lower than the national average. The risk of tornado damage in Bay City Independent School District is much lower than Texas average and is about the same as the national average.

Topics:Earthquake IndexVolcano IndexTornado IndexOther Weather Extremes EventsVolcanos NearbyHistorical Earthquake EventsHistorical Tornado Events

Earthquake Index, #993

Bay City Independent School District
0.00
Texas
0.04
U.S.
1.81

The earthquake index value is calculated based on historical earthquake events data using USA.com algorithms. It is an indicator of the earthquake level in a region. A higher earthquake index value means a higher chance of an earthquake.

Volcano Index, #1

Bay City Independent School District
0.0000
Texas
0.0000
U.S.
0.0023

The volcano index value is calculated based on the currently known volcanoes using USA.com algorithms. It is an indicator of the possibility of a region being affected by a possible volcano eruption. A higher volcano index value means a higher chance of being affected.

Tornado Index, #968

Bay City Independent School District
131.49
Texas
208.58
U.S.
136.45

The tornado index value is calculated based on historical tornado events data using USA.com algorithms. It is an indicator of the tornado level in a region. A higher tornado index value means a higher chance of tornado events.

Other Weather Extremes Events

A total of 1,036 other weather extremes events within 50 miles of Bay City Independent School District were recorded from 1950 to 2010. The following is a break down of these events:

TypeCountTypeCountTypeCountTypeCountTypeCount
Avalanche:0Blizzard:0Cold:1Dense Fog:0Drought:39
Dust Storm:0Flood:186Hail:284Heat:8Heavy Snow:2
High Surf:0Hurricane:4Ice Storm:2Landslide:0Strong Wind:1
Thunderstorm Winds:397Tropical Storm:7Wildfire:6Winter Storm:2Winter Weather:2
Other:95 

Volcanos Nearby

No volcano is found in or near Bay City Independent School District.

Historical Earthquake Events

No historical earthquake events that had recorded magnitudes of 3.5 or above found in or near Bay City Independent School District.

No historical earthquake events found in or near Bay City Independent School District.

Historical Tornado Events

A total of 27 historical tornado events that had recorded magnitude of 2 or above found in or near Bay City Independent School District.

Distance (miles)DateMagnitudeStart Lat/LogEnd Lat/LogLengthWidthFatalitiesInjuriesProperty DamageCrop DamageAffected County
4.61961-09-11229°00'N / 95°54'W0.40 Mile50 Yards000K0Matagorda
17.21953-12-02229°12'N / 96°02'W1.50 Miles200 Yards003K0Wharton
21.81969-04-11328°48'N / 95°39'W2.00 Miles67 Yards0132.5M0Matagorda
23.61970-10-23229°18'N / 96°00'W1.20 Miles33 Yards0025K0Wharton
23.71967-09-20328°42'N / 96°13'W1.00 Mile100 Yards4725K0Matagorda
23.81970-10-23229°18'N / 95°54'W1.50 Miles27 Yards0025K0Wharton
24.41955-05-18228°42'N / 96°14'W2.50 Miles33 Yards0025K0Matagorda
25.01964-06-15229°18'N / 96°06'W1.50 Miles20 Yards003K0Wharton
25.01966-04-14229°18'N / 96°06'W1.00 Mile33 Yards000K0Wharton
25.71955-05-23229°19'N / 96°05'W0.50 Mile33 Yards000K0Wharton
26.81972-03-20229°20'N / 96°05'W0.50 Mile50 Yards0025K0Wharton
31.31961-11-22329°24'N / 96°05'W2.00 Miles200 Yards010K0Wharton
31.71966-04-18329°04'N / 95°27'W2.00 Miles50 Yards000K0Brazoria
32.81975-12-24329°01'N / 96°30'W1.00 Mile440 Yards000K0Jackson
33.91965-04-19329°27'N / 96°00'W0.20 Mile150 Yards1325K0Fort Bend
34.41967-09-20329°04'N / 96°31'W0.10 Mile33 Yards030K0Jackson
36.61966-03-28329°27'N / 96°20'W29°23'N / 96°12'W9.30 Miles1760 Yards0025K0Colorado
37.11993-04-07229°25'N / 96°17'W0.50 Mile400 Yards0050K0Wharton
 Brief Description: The Wharton Newspaper reported large trees blown down, metal roofs blown off barns and water pump housings blown over on Farm-to-Market Road 2614 northwest of Egypt near the community of Bonus. There were numerous reports of street flooding in the Wharton vicinity.
37.41981-05-09229°30'N / 95°49'W29°28'N / 95°47'W3.30 Miles40 Yards0025K0Fort Bend
42.71966-02-09328°58'N / 96°40'W2.00 Miles33 Yards0025K0Jackson
46.21961-11-02228°37'N / 96°37'W0.30 Mile200 Yards0025K0Calhoun
46.21972-05-07228°37'N / 96°37'W0.10 Mile10 Yards0125K0Calhoun
46.31974-09-13329°35'N / 95°45'W29°37'N / 95°43'W3.60 Miles73 Yards020K0Fort Bend
46.91970-08-03228°24'N / 96°24'W003K0Calhoun
48.91976-03-08329°22'N / 95°26'W29°27'N / 95°14'W13.40 Miles200 Yards0182.5M0Brazoria
49.41964-02-04229°36'N / 96°20'W29°37'N / 96°17'W3.80 Miles880 Yards01250K0Colorado
49.42003-11-17229°37'N / 95°38'W29°37'N / 95°38'W1.50 Miles200 Yards060500K0Fort Bend
 Brief Description: Tornado touched down on west Airport Drive near Industrial in Sugar Land. 60 injuries with 7 people sent to hospital for further treatment. Damage to several office building roofs in Industrial Park. Additional damage to a Daycare facility at West Airport Drive and Dairy Ashford Road. Roof damage to several residential homes in the Meadows subdivision. Reports of several cars overturned or blown off of road along Airport Drive. A total of 24 tornadoes touched down during this 15 hour period of severe weather in southeastern Texas on November 17, 2003. In addition to these tornadoes, a major flood developed over Harris and surrounding counties during the middle of this tornadic outbreak. Over 300 homes, along with hundreds of vehicles, were flooded. These tornadic storms developed over parts of Wharton and Matagorda counties shortly after sunrise with the first confirmed tornado occurring just east of El Campo around 9:00 am. Strong 500mb upper level troughing over the western U.S. moved from west to east across the Southern Plains. The polar jet stream associated with this 500 millibar trough surged into west Texas and then curved sharply northeastward into the Central Plains. The sub-tropical jet stream was oriented west to east across deep southern Texas. This jet stream pattern was the impetus to strong lower level convergence due to the enhanced upper level divergence. Low level moisture had substantially increased and was about 200 percent of normal by 6 AM. Vertical wind profiles also showed a great deal of low level wind shear with the greatest shear occurring in the lowest 2000 feet. In addition, these veering wind speeds rapidly increased with height. A focus for the thunderstorm development was provided by a weak low level boundary which was aligned southwest to northeast, or generally along the U.S. Highway 59 corridor. This feature was nearly-stationary and thunderstorms repeatedly developed and moved along this boundary. The axis of heaviest rain was coincident with this boundary.


* The information on this page is based on the global volcano database, the U.S. earthquake database of 1638-1985, and the U.S. Tornado and Weather Extremes database of 1950-2010.


 
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