Instructional Materials on Making Weather Observations

Adapted to the World Wide Web from a file on the University of Michigan Gopher. Another adaptation was done on a file describing a Weather Forecasting Contest for the schools in which the students use the real-time weather information on the Michigan Weather Underground.

This file contains the procedure on how to make a weather observation. It also contains sources (phone numbers) on where to get information on weather instruments.

Procedure for making a weather observation.

Temperature :

Use a thermometer and read it to the nearest integer. Do not measure temperature directly in the sun or very close to the ground.

Clouds :

Type - Cloud charcteristics vary depending on their altitude as well as the atmospheric conditions.

Altitude:

Low clouds: Stratus (dull gray,usually overcast, associated with steady precipitation). Some other species of low clouds include nimbostratus, cumulus, stratocumulus, mamatocumulus.

Middle clouds: Begin with the prefix alto. Examples include altocumulus, altostratus.

High clouds: Cirrus, cirrocumulus, cirrostratus. Usually appear "feathery".

Weather conditions:

Many times you can identify the current (or future) weather situation by analysis of cloud type and coverage, for example: Cirrus clouds are fair weather clouds, they usually indicate an approaching front. Cumulonimbus clouds are indicative of significant upward motion (due to warm humid air at the surface rising, then condensing) that leads to thunderstorm development (convection). Stratus clouds are good indicators that precipitation is approaching. Brief descriptions of some cloud types.

Stratus

The uniform dull gray colored clouds that often cause completely overcast skies. The gray underside of the cloud is shapeless and may resemble fog. The clouds are layered and formed largely from the nearly horizontal motion of air with one air layer slidding over another. These clouds are found at low altitudes.

Stratocumulus

Clouds that consist of masses or rolls of cumulus clouds, usually arranged in a pattern with narrow breaks between the individual clouds. They often form "cigar shaped" rolls. The bases of the clouds form at low altitudes. They are common in the late fall and winter.

Cumulus

Detached clouds, generally dense and with sharp outlines, developing vertically in the form of rising mounds, domes or towers, of which the bulging upper part often resembles a cauliflower. The sunlit parts of these clouds are mostly brilliant white; their base is relatively dark and nearly horizontal. Expansion of rising air results in adiabatic cooling thus forming cumulus clouds.

Nimbostratus

Grey cloud layer, often dark, the appearance of which is rendered diffuse by more or less continuously falling rain or snow. The clouds are shapeless and of a low altitude. Slow steady rain or snow may develop from these clouds.

Altocumulus

Clouds found at middle altitudes that are similar in appearance to cumulus clouds. Altocumulus clouds are composed of white or gray, rounded patches with sky visible between the patches. These clouds are often arranged in groups or lines.

Altostratus

Middle altitude stratus clouds. They are smooth on the underside forming a uniform gray sheet. The faint image of the sun can sometimes be seen through them. These clouds sometimes appear bluish.

Cumulonimbus

Heavy and dense cloud with a considerable vertical extent, in the form of a mountain or huge towers. The upper portion of the cloud spreads out in the shape of an anvil. Under the base of this cloud (which is often very dark) there are frequently low ragged clouds either merged with it or not, and precipitation sometimes in the form of virga.

Mamatocumulus

These clouds extend downward from a cumulonimbus cloud, they appear as bubble like bulges. They are formed by a cold downdraft near the edge of a thunderstorm and as a result can accompany severe weather conditions and in particular tornadoes.

Coverage

Cloud coverage is classified into the following four categories.

Movement

Clouds move in the direction the wind is blowing at the altitude of the clouds. Clouds can be moving a different direction than the observed wind at the surface. If a cold front just passed through the winds will be backing with height (counterclockwise shift in wind direction). If a warm front is approaching the winds will be veering with height(clockwise shift in wind direction).

Precipitation:

Rainfall is recorded by a rain gauge. Snowfall can be measured by using a ruler to record the depth. Precipitation amount is always given as the amount of precipitation that fell over a given time period (generally 24 hours, midnight to midnight). If the precipitation occurs while the wind is strong precipitation measurements must be measured carefully. Rain would fall more horizontally which means the instrument wouldn't "catch" all the rain that actually falls. Snow depth would vary considerably because of drifting so measure the depth at many flat, open locations and take an average estimate. In making an observation while there is precipitation, note the time precipitation began and ended.

Wind:

Wind has a speed and a direction. Wind speed is measured by an anemometer. Wind direction can be estimated by noting which way a flag is blowing. Remember wind direction is taken as the direction the wind is coming from.

Present weather:

Weather is constantly changing and can change in many different ways.

Is it precipitating, if so, what kind of precipitation is it (rain, snow, ice pellets, hail, mix) and what is the intensity of the precipitation (light, moderate or heavy). Visibility is generally a good indicator of precipitation intensity. Note the distance to landmarks near the observation spot and determine what landmarks are visible when there is significant precipitation.

Is the precipitation associated with a thunderstorm, if so the intensity of the thunderstorm should be noted. Is there lightning associated with the thunderstorm, if so how what is the intensity (frequent or occasional, cloud to cloud or cloud to ground). Is there hail with the thunderstorm, if so what is the size of the hail (its diameter). Is there a tornado associated with the thunderstorm. Sources for weather instruments.

Nimbus instruments                     1-800-633-1033
The Weather Store                      (617) 742-3045
Weather Station                        1-800-321-9542
American Weather Enterprises           (215) 565-1232
Wind and Weather                       (707) 964-1284
Texas Weather Instruments              1-800-284-0245
Meteophysics Corp.                     (415) 331-5181
Texas Electronics Inc.                 (214) 631-2490
Maximum Inc.                           (508) 995-2200
Magnaphase Industries, Inc.            (206) 735-0374
They have many different weather instruments: Thermometers, rain gauges, wind measuring instruments, to name a few. Prices are highly variable.