When the temperatures become hot, water vapor condenses from nearby water sources and around mountain tops, forming dark clouds. These clouds have the potential to culminate in intense electrical storms.
Clearly, it is unwise to continue ascending a summit as the sky pulsates with gigantic bolts of lightning, but sometimes the situation is unavoidable. You may not know that a storm is coming until it crests the summit towards which you may be ascending. In those cases, there are safety measures you can take to protect yourself. Nevertheless, you can reduce your chances of becoming caught off guard by surprise storms as you become a better observer of the sky. Here we’ll help you learn how to become a better observer of the sky, so the next time you are headed to an open area, you can more accurately predict if a thunderstorm is approaching.
To fully appreciate the phenomenon of weather, you must first understand how it happens.
The atmosphere is filled with water vapor from the evaporation of water covering the earth’s surface and the ocean. As the water-filled air (or vapor) rises, cools, and condenses (moves from a warm place to a cool place), it forms into water droplets or clouds. A cloud is merely a collection of minute water droplets or ice crystals. Small hygroscopic particles in the sky, such as dust, sea salt, smoke, and airborne pollutants, are attracted to water and are absorbed by a cloud’s water droplets. These water droplets come together and form into clouds.
Not all clouds produce precipitation. The water droplets fall from the clouds when they become too heavy to remain suspended in the air. Similar to how humans release toxins through sweat and excretion, the process of clouds and precipitation (rain, snow, or hail) are nature’s way of cleansing the atmosphere of accumulating particulates. This is one reason why increased pollution and warming of the Earth’s atmosphere bring about a greater frequency of extreme weather events.
Sometimes the rain never reaches the ground, even when rain clouds appear. If the lower atmosphere is dry, common in cooler temperatures and arid regions, precipitation may evaporate before it reaches the ground. This explains why rain often shows up on the radar image, but no rainfall is recorded at ground level.
Clouds take on different appearances depending on what is happening in the atmosphere. Once you learn the characteristics of clouds, you can predict the weather more accurately.
Billowing cumulus clouds in the afternoon indicate fair weather. If they grow into nimbus, they indicate fast storms. The likelihood of cumulus clouds developing into nimbus clouds increases as the atmosphere warms up in the summer, especially in the afternoon hours (between 3 – 6 PM).
The size and shape of clouds provide you a tool to accurately predict the weather. When taken together, they indicate the likelihood of precipitation.
All of this means nothing unless you know what the cloud shape represents. The best way to learn is to memorize the cloud shapes and identify them the next time you are outside. As you make a habit of staring into the sky, you’ll start to notice what shapes produce precipitation.
Clouds are identified and categorized by several factors: the altitude of the cloud, the cloud shape, texture, vertical extent, color, and whether or not the cloud is producing precipitation. The World Meteorological Organization (WMO) classifies the height and shape of clouds using Latin prefixes and suffixes. Combine the 3 terms – shape, elevation, and precipitation – and you are cloud conversant.
Clouds described by Elevation
Clouds described by Shape
Clouds described by Precipitating
Clouds do not always tell the full story of forthcoming weather. You also need to examine the wind. The wind is another useful indicator of bad weather because it is created from disorder in the atmosphere. If the wind suddenly picks up, towering cumulus clouds build vertically and begin to darken, you should consider hiking away from summits and exposed ridge tops.
Nature is all about balance. Regions of excess move toward regions of deficit. As warm air rises, air pressure drops. That is because when air rises, the air molecules move away from the surface causing a low pressure at the surface. The surrounding air moves to the surface to replace the warm air that has risen. The earth tries to balance surface pressure by moving high pressure (colder) air to low pressure (warmer) areas under rain clouds. When these air masses of differing pressures meet, “wind” is created. The wind serves to equalize the pressure between the two different air masses by moving the air away.
In addition to clouds and wind, a dropping of barometric pressure can identify the likelihood of a storm. A storm is undoubtedly forthcoming when the wind suddenly picks up, dark clouds hover above your head, and the air pressure drops. You should no longer consider descending down a summit, but do it!
How can you tell if the pressure is dropping? Most altimeters work by measuring barometric pressure. When the barometric pressure rapidly drops, it often means a change for the worst. You can get an indication of these changes by the fact that your elevation suddenly begins to change far more rapidly than the known elevation of the trail. This is not an exact science, though. As altitude increases, atmospheric pressure decreases. But a sudden drop in temperature, such as from a cold front, can make the reading inaccurate. That is because most devices that measure barometric pressure rely on “density altitude” or mass of air which varies based on temperature and humidity.
Not every hiker carries an altimeter with them, and many don’t find a need to do so. However, a barometric altimeter is a pretty simple device, and many multi-function sports watches (i.e., the Casio Solar) and survival knives have this feature. We’ve found the altimeter useful on many occasions because it helps identify your location when used with a topographic map.
Keep in mind that barometric pressure changes with the weather and must be re-calibrated every so often when the altitude is known. Most wilderness areas display the altitude at various trail junctions or atop mountain peaks.
If you have an altimeter, always check the altitude reading to a known altitude printed on a map or trail marking.
GPS altimeters may also work but tend to be less accurate when hiking in areas with a weak satellite signal or hiking deep down in areas such as gorges or canyons.
If you do not have a scientific way to measure barometric pressure, you can look for signs in nature. Birds have a tendency to fly much lower to the ground right before rain due to the thinning of the air. Most people also report having an increased sense of smell. If you are hiking in a damp or swampy area and the air seems to become stinkier or smell like compost, expect rainy weather. That is because swamps and plants release gases as the pressure decreases. Other people can “feel” rain approaching due to an increased sensation of pain in their joints or sinus pressure.
Why pressure changes in response to weather
The weight of the air pressing down on the Earth causes air pressure. The “weight” or amount of Barometric Pressure changes based on several factors, including the air temperature, altitude, and humidity. Cold air has a higher mass than warm air, which creates a different pressure. Low pressure is associated with bad weather because less pressure causes the air to rise. The rising air cools and causes condensation, which releases water in the form of rain.
Familiarity with weather lore is also helpful for predicting the weather. Not all of these sayings hold true for all circumstances, but many are surprisingly accurate.
Looking at the Moon
Looking at the Sun
Looking at Rainbows
Looking at Wildlife
Birds and insects tend to fly much lower to the ground before rain due to the thinning of the air. If you have a campfire, you’ll also notice the smoke hovers nearer to the ground for the same reason.
Look at Plants
Learning how to read cloud formations is a useful wilderness skill because clouds are a good indicator of approaching weather. Cell phones and other electronic devices are not always useful or reliable in remote wilderness areas because forecasting is often imprecise or irrelevant for your exact location. And as the Earth’s atmosphere warms up due to the increased concentration of greenhouse gases, it brings about a greater frequency of extreme weather events. Taking the time to understand how the weather happens can help you prepare for these sudden storms. Now that you understand how all of this works, you are a knowledgeable weather observer.
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