Picture Banner for SECC K12 Site

Extremes body


 

Extreme Weather
Figure A
Image from www.sun-tek.com

An extreme weather event is a type of event that doesn't occur very often. Generally, extremes occur less than 5 percent of the time when you look at the entire climate record (in statistical terms, more than 2 standard deviations away from average). Examples of extreme events include unusually heavy rainfall amounts in a short period of time, periods of drought, outbreaks of frigid temperatures, or unseasonal weather. These events typically affect relatively small areas but may become widespread if similar conditions like hot temperatures are experienced over a wide region.  In that case many individual station records can be set on a single day.

Many scientists believe that extreme weather events appear to be on the increase.  Some of this may be due to changing land conditions at the location of individual weather stations, since as areas become more urbanized the amount of pavement increases and causes temperatures to become warmer as well as increasing runoff from thunderstorms.  However, even in rural areas far from growing cities, the number of record-setting events  does not seem to be decreasing even as the station records get longer.

Extremes of temperature include record high and low temperatures, but can also include the record high minimum temperature (usually observed near dawn of a warm night) and the record low maximum temperature (on the afternoon of an unseasonably cold day).  Temperature records can also include monthly averages and runs of days with temperatures above a certain threshold like 100 degrees or below freezing.  Temperatures below freezing are especially critical since that is the temperature at which damage to crops becomes much more likely due to ice development inside of the plant cells.  Some plants also stop growing when temperatures above a value like 90 degrees are reached.

Rainfall can have three separate extreme values: duration of rainfall, intensity of rainfall, and the accumulation of rainfall.  These records are most often kept for daily and monthly amounts in climate studies, but can be kept for any time period that the rain gauge is capable of measuring. Rainfall is somewhat different than temperature in extremes because rainfalls of zero are quite common over short time periods, whereas temperatures tend to occur over a range equally spread between values above and below the long-term average.

Extreme rainfalls can occur under a number of different weather conditions.  Small areas of rain can be hit by intense thunderstorms and a lot of rain can accumulate over a short time period, especially if new thunderstorms develop and move over the same location (this is called "training" since the storms follow each other along the same track).  Sometimes extreme rainfall amounts can occur while hurricanes and tropical storms are making landfall or moving slowly over land. 

When rain falls continuously over the same area for long time periods, significant floods can result.  The ground can only absorb a certain amount of rain each hour, and once it is saturated the rain has nowhere to go but to run off into the rivers, which can flood if too much water reaches them at once.  In northern areas, flooding can also occur if snow on the ground melts rapidly when hit by warm air or warm rain, especially if the ground is already saturated.

The 100 year storm

Engineers use statistical information about rainfall and flooding to estimate how often a given amount of rain is likely to occur.  A 100-year storm is a rainfall event that has a statistical probability of a one percent chance of occurring in any given year. Over a long time, this would mean that a storm of this magnitude would occur on average once every 100 years.  However, since a storm this strong has a one percent chance of occurring each year, it is possible to have two 100-year storms in less than 100 years, at a given location. Almost every state has at least one 100-year storm occur somewhere inside the state each year, just at different locations over time. 

The 25 & 50-year storms are also storms that occur in the same way. A 25-year storm is likely to occur in an area once every 25 years which means that there is a four percent chance of a storm of this magnitude occurring on any given year. A 50-year storm would be likely to occur once every fifty years, or has a two percent chance of occurring on any given year. A rainfall amount that occurs on average once a year is said to have a 1-year return period, or recurrence interval, whereas a storm that on average occurs once every hundred years is said to have a 100 year return period. Each storm is associated with a time of accumulation, so you would have separate rainfall amounts for a 100-year 1-hour storm than you would for a 100-year 24-hour storm.

A return period, or recurrence interval, is a statistical measurement used to estimate the amount of time between two extreme events of the same magnitude (i.e. 100-year storm, 100-year flood, extreme rainfall event, major hurricane, ...). Hydrologists  use return period to determine the likelihood of occurrence of an extreme rainfall event. Return periods are also used in risk analysis for determining the risk for building projects, such as highways and bridges, in areas of particular risk of having an extreme rainfall event occur. Optimal return periods vary with the type of project, the drainage area around the pending project, and the risk of failure of the structure.

Below is a chart showing the likelihood that one of these events (storm or flood) would occur and the percentage they could occur in any given year.

Storm Interval Occurrence
Figure B
Image from USGS

Similar to a 100-year storm is a 100-year flood. Just like extremely heavy rain, it is possible for a 100-year flood to occur more than once in 100 years.  A 100-year storm does not always lead to a 100-year flood, but both of these extreme events occur with the same interval of frequency.  A 100-year flood takes into account both the effects of heavy rainfall, the saturation of the soil, and the amount of pavement in the area over which the rain is falling.  So a 100-year rain falling on ground that is very dry and unpaved is less likely to cause flooding than a 25-year rain that falls on ground that is already saturated from an earlier rain event and has a lot of pavement on it.

Rainfall statistics like these are used in the design of roads, catchment basins, dams, and nuclear power plants.  These structures need to be able to withstand extremely heavy rains and remain safe to use.  An interstate highway is designed to drain a more extreme storm than a local city street since traffic is more vulnerable at higher speeds.  Dams are often designed with an extra flood control capacity included in how much water is allowed to be stored behind the dam, since too much water in the reservoir (from a slow-moving tropical storm, for example) could top the dam and wash it out, causing massive damage and even loss of life downstream.

Urban Development Impacting Flood Region

Figure C
Image from USGS

Figure C shows how urban development has impacted the 100-year flood level at Mercer Creek near Bellevue, Washington. Figure D shows how dams have helped lower the level of the 100-year flood at Green River near Auburn, Washington.

Dams Impacting Flood Level

Figure D
Image from USGS

Last modified date: Tuesday, August 7, 2012 - 10:34am