A Vital Factor In Weather
It's no secret that the earth and its atmosphere get their warmth from the sun. However, the relationship of the sun to the earth is such that the earth and its atmosphere are heated unevenly, resulting in a variation of temperatures. This heating is the fundamental cause of winds, storms, clouds, rain and snow.
The temperature of air affects air pressure, determines the amount of water vapor a specific volume of air can hold and is responsible for rising and descending air currents. Since temperature is such a vital factor in these weather conditions, it is helpful to thoroughly understand it and its effects.
The Most Vertical Rays Of The Sun Are The Hottest!
We can determine this from several observations. First, the sun's rays are hotter at noon, when they are most vertical or perpendicular to the earth's surface, than at sunrise or sunset when they are slanted. Second, it is hotter at the equator than at the north and south poles. Rays of the sun are most vertical at the equator and least vertical at the poles. In the northern hemisphere, the sun's rays are strongest in June when they are most vertical and much weaker in December when they are least vertical.
There are two reasons why the sun's rays are strongest and therefore warmest when they are most vertical. These can be seen in the diagram shown.
First, perpendicular or vertical rays pass through less atmosphere than slanted rays. As a result, they pass through less energy-absorbing impurities, such as dust, and arrive at the earth's surface with more energy. Second, the energy from the rays concentrates in a limited area, like the beam of a flashlight that is directed at the floor. If the rays are slanted (or the flashlight tilted), the same energy is spread over a much larger surface area. Each given area then receives a smaller portion of the total energy.
What Happens To The Sun's Energy?
The sun's rays do not always heat the objects they encounter. For example, the sun's rays go right through a transparent material, such as glass, without heating it. When the sun's rays strike shiny surfaces, such as mirrors, the rays are reflected. Those objects also are not heated. Only when the rays of the sun are absorbed are they converted into heat.
In general, solids are better heat-absorbers than liquids, while dark rough objects absorb heat better than light-colored, smooth objects. This explains why sand (a solid) at the beach gets hotter than the ocean (a liquid) in the afternoon, and why people wear light-colored clothing in the summer and darker clothing in the winter.
Easy come, easy go! Objects that heat up quickly also cool off quickly. At the beach, the sand heats up quickly during the afternoon while the water heats up very slowly. At night, the sand quickly loses the heat it gained during the afternoon and is much cooler than the adjacent water. Consequently, on a hot summer day, it is a good idea to head for water in order to cool off. Since it takes water a long time to heat and cool, the ocean or lake remains cool from the previous winter. During the winter, though, coastal sections and locations near a lake have milder weather, since the water retains some of the heat acquired during the previous summer. This explains why coastal sections get rain during the winter while inland areas, away from the warm influence of the ocean waters, get snow. Likewise, easy come, easy go means inland sections generally have hotter summers and colder winters, while coastal locations adjacent to an ocean or large lake have cooler summers and milder winters.
Generally the "bottom" air of the atmosphere is warmest since it receives heat from the earth's surface. Remember, the sun's rays are absorbed by dark, solid objects such as soil. This heat is transferred to the air just above it. Also, since the atmosphere is denser (more molecules of air per unit of space) near the earth's surface, it absorbs the sun's rays more than the thinner, upper levels of the atmosphere. This explains why the mountains also are good places to cool off during summer heat waves. Generally, air temperatures drop approximately 3 1/2°F for every 1000 feet of elevation. These cooler mountain temperatures also produce more snow than at lower elevations, where temperatures may be warm enough to produce rain.
Heat is transferred through the atmosphere in three ways.
Rays of the sun pass through space or transparent objects (e.g. energy from the sun to the earth).
Heat is transferred by actual contact. Hot objects touching other objects will pass heat to them. If the ground is hot, the air immediately above it will become hot by coming into contact with the heated ground.
Heat is actually "carried" from one part of the atmosphere to another. This transfer is accomplished by currents within the heated material as shown in the diagram below.
is applied at the bottom. The heated
material above the flame rises. Colder fluid
sinks on the opposite side then flows toward the
candle side to replace the rising fluid. A
"convection current" is formed.
Later we will
show how rising and sinking air currents
are responsible for much of our weather -
both good and bad.
Forecasting Temperature: What Factors Must Be Considered
When the sun's rays hit clouds, they are reflected back into space, never reaching the ground. Thus, cloudy days are cooler than sunny days. However, at night clouds act as a "blanket" preventing heat loss from the earth. As a result, cloudy nights generally are warmer than clear nights. The temperature range, the difference between the highest and lowest temperature in any day, is smallest during cloudy periods.
When winds are very light or calm, the air molecules near the earth's surface move very little and are able to remain in contact with the ground below. On a sunny day the ground absorbs the sun's rays and heats up, so the air in contact with the ground is heated. At night, since the ground cools off quickly, air in contact with the cold ground cools rapidly also. Thus, during periods with nearly calm winds and clear skies, daytime temperatures are warm and nighttime temperatures are cold. A larger temperature range occurs. During windy weather, daytime temperatures do not climb as high, and, more importantly, nighttime readings do not drop as low, making for smaller daily temperature ranges.
3. MOISTURE AND CARBON DIOXIDE:
The term humidity is generally used to refer to the moisture condition of the atmosphere. If the atmosphere contains a great deal of moisture (high humidity) nighttime temperatures remain mild. This is so because water retains its heat. Therefore, temperature ranges between day and night are greatest when the air is dry (low humidity) and least when the air is moist.
Although it is only a tiny fraction of the earth's atmosphere, carbon dioxide decisively influences the heat balance. Since it possesses a property similar to that of glass, it is transparent to radiation coming from the sun. However, it traps radiation or heat given off by the earth. This captured heat warms the lower atmosphere, preventing strong nighttime cooling. Carbon dioxide levels are highest near industrial sections since carbon dioxide is the by-product of combustion, a common manufacturing process. The atmosphere surrounding large cities contains higher concentrations of carbon dioxide, thus nighttime cooling in large cities is less than in surrounding areas.
4. SNOW COVER:
Daytime temperatures are lower in areas of snow cover since some of the sun's rays are reflected back into space when they encounter this smooth, white surface. At night, snow radiates rapidly whatever heat it has gained. As a result, nighttime temperatures can drop significantly in areas covered by snow.
To sum up:
Coldest nights often occur with cloudless skies, little or no wind, low humidity, and snow cover. Warmest days normally occur with cloudless skies, little wind, low humidity, and the ground free of snow cover.
We discussed earlier that it is normal for "bottom air" near the ground to be warmest. Temperatures normally get colder higher in the atmosphere. However, there are occasions when the bottom air is cooler than the air above. When this happens we have a temperature inversion. It occurs most commonly on nights that are clear, calm, and dry. The ground cools off rapidly by radiation, subsequently cooling the air near the ground by conduction. The cold air near the ground, being denser and heavier, stays where it is. The warmer air above, being less dense and lighter, does not sink and make contact with the cold ground. The result is a lack of vertical movement. Convection cannot take place! Under these circumstances, pollutants are trapped near the surface and unhealthy air-quality conditions may result.
Temperature inversions are broken when the sun's rays are able to heat the earth's surface, which in turn heats the bottom air that begins to rise. A convection current is established. As we will show later, temperature inversions often are responsible for certain types of precipitation.
How Is Temperature Measured?
We all know that the instrument used to measure temperature is the thermometer. But there are several types of thermometers. The liquid version uses mercury or alcohol in a glass column. These liquids expand at a uniform rate as heat increases. Alcohol is used in extremely cold climates since mercury freezes at -39°F and would be useless at temperatures below that. The freezing point of alcohol is -200°F. No place on earth ever gets that cold! (Record worldwide low temperature is -127°F, Vostok, Antarctica.)
Thermometers also can be composed of a dual metallic strip that expands and contracts at varying degrees, causing the strip to bend up or down as the temperature rises or falls. Modern digital thermometers use solid-state electronics to indicate air temperature.
Temperature can be expressed either in degrees Fahrenheit or degrees Celsius. These simple formulas convert one scale to the other.
To convert a Fahrenheit reading to Celsius. use the formula:
°F = Fahrenheit Temperature
°C = Celsius Temperature
A Fahrenheit reading of 77° = 25°C
°C = 5/9 (77° — 32°)
°C = 5/9 X 45° = 25°C
To convert a Celsius reading to Fahrenheit, use the formula:
°F =9/5°C + 32°
To convert 25°C back to degrees Fahrenheit:
°F = 9/5 x (25°) + 32°
°F = 45° + 32° = 77°F
Indicating Temperatures On Weather Maps
1. THE STATION MODEL:
Weather observations are taken hourly in all large cities and airports and relayed via high-speed internet circuits to computers in Washington, D.C., and Kansas City, Missouri. From here they are transmitted nationwide and worldwide. Meteorologists and computers then can record this data on appropriate station models shown on a large map. A station model is a circle on a map representing a weather station, usually identified by three letters or numerals. Weather conditions are shown with numbers or symbols at specific locations around this circle. For example, in the diagram, temperature is placed next to the upper left-hand area of the circle.
2. KEEPING TRACK
Meteorologists use heating degree days to determine how cold a winter is, compared with the previous winter. Heating degree-days are calculated for days having a mean temperature below 65°F. Such days are considered to require indoor heating. Degree-days are calculated by subtracting the daily mean temperature (the daily high + the daily low)/2 from 65°F. Mean temperatures 65°F or higher are listed as zero.
If on a particular day the temperature ranged from 30°F to 60°F, the mean temperature for the day would be (30° + 60°)/2 = 45°F. Such a day is said to have 20 degree-days (65 - 45 = 20). Colder days result in more degree-days and more fuel consumption.
The map indicates the average annual umber of degree-days across the United States.