| | The Water Cycle: Water Storage in the Atmosphere The atmosphere is full of water Credit: Chris Picking The water cycle is all about storing water and moving water on, in, and above the Earth. Although the atmosphere may not be a great storehouse of water, it is the superhighway used to move water around the globe. Evaporation and transpiration change liquid water into vapor, which ascends into the atmosphere due to rising air currents. Cooler temperatures aloft allow the vapor to condense into clouds and strong winds move the clouds around the world until the water falls as precipitation to replenish the earthbound parts of the water cycle. About 90 percent of water in the atmosphere is produced by evaporation from water bodies, while the other 10 percent comes from transpiration from plants. There is always water in the atmosphere. Clouds are, of course, the most visible manifestation of atmospheric water, but even clear air contains water—water in particles that are too small to be seen. One estimate of the volume of water in the atmosphere at any one time is about 3,100 cubic miles (mi3) or 12,900 cubic kilometers (km3). That may sound like a lot, but it is only about 0.001 percent of the total Earth's water volume of about 332,500,000 mi3 (1,385,000,000 km3), as shown in the table below. If all of the water in the atmosphere rained down at once, it would only cover the globe to a depth of 2.5 centimeters, about 1 inch. The little cloud that could—but why? (Why does this cloud exist?) How much does a cloud weigh? Do you think clouds have any weight? How can they, if they are floating in the air like a balloon filled with helium? If you tie a helium balloon to a kitchen scale it won't register any weight, so why should a cloud? To answer this question, let me ask if you think air has any weight—that is really the important question. If you know what air pressure and a barometer are, then you know that air does have weight. At sea level, the weight (pressure) of air is about 14 ½ pounds per square inch (1 kilogram per square centimeter). Since air has weight it must also have density, which is the weight for a chosen volume, such as a cubic inch or cubic meter. If clouds are made up of particles, then they must have weight and density. The key to why clouds float is that the density of the same volume of cloud material is less than the density of the same amount of dry air. Just as oil floats on water because it is less dense, clouds float on air because the moist air in clouds is less dense than dry air. We still need to answer the question of how much a cloud weighs. To confuse things more, the weight depends on how you define it: - The weight of the water droplets in the cloud
- The weight of the water droplets plus the weight of the air (mostly above the cloud, pressing down)
We're only going to look at the weight of the actual cloud particles, and realize different clouds have varying densities of cloud particles (and, thus, different weights). Let's use your basic "everyday" cloud—the cumulus cloud with a volume of about 1 cubic kilometer (km) (0.62 miles) located about 2 km (1.2 miles) above the ground. In other words, it is a cube about 1 km (0.24 cubic miiles) on each side. One measurement (http://snowball.millersville.edu/~adecaria/ESCI340/esci340_cp_lesson01_cloud_properties.pdf) of cumulus-cloud density is about 0.5 gram per cubic meter. A 1 km3 cloud contains 1 billion cubic meters. Doing the math: 1,000,000,000 x 0.5 = 500,000,000 grams of water droplets in our cloud. That is about 500,000 kilograms or 1.1 million pounds (about 551 tons). But, that "heavy" cloud is floating over your head because the air below it is even heavier— the lesser density of the cloud allows it to float on the dryer and more-dense air. Global distribution of atmospheric water One estimate of global water distribution Water source | Water volume, in cubic miles | Water volume, in cubic kilometers | Percent of total freshwater | Percent of total water | Atmosphere | 3,094 | 12,900 | 0.04% | 0.001% | Total global fresh water | 8,404,000 | 35,030,000 | 100% | 2.5% | Total global water | 332,500,000 | 1,386,000,000 | -- | 100% | Source: Gleick, P. H., 1996: Water resources. In Encyclopedia of Climate and Weather, ed. by S. H. Schneider, Oxford University Press, New York, vol. 2, pp.817-823. | |
| Precipitation: The Water Cycle Precipitation is water released from clouds in the form of rain, freezing rain, sleet, snow, or hail. It is the primary connection in the water cycle that provides for the delivery of atmospheric water to the Earth. Most precipitation falls as rain. How do raindrops form? The clouds floating overhead contain water vapor and cloud droplets, which are small drops of condensed water. These droplets are way too small to fall as precipitation, but they are large enough to form visible clouds. Water is continually evaporating and condensing in the sky. If you look closely at a cloud you can see some parts disappearing (evaporating) while other parts are growing (condensation). Most of the condensed water in clouds does not fall as precipitation because their fall speed is not large enough to overcome updrafts which support the clouds. For precipitation to happen, first tiny water droplets must condense on even tinier dust, salt, or smoke particles, which act as a nucleus. Water droplets may grow as a result of additional condensation of water vapor when the particles collide. If enough collisions occur to produce a droplet with a fall velocity which exceeds the cloud updraft speed, then it will fall out of the cloud as precipitation. This is not a trivial task since millions of cloud droplets are required to produce a single raindrop. A more efficient mechanism (known as the Bergeron-Findeisen process) for producing a precipitation-sized drop is through a process which leads to the rapid growth of ice crystals at the expense of the water vapor present in a cloud. These crystals may fall as snow, or melt and fall as rain. Care to guess how many gallons of water fall when 1 inch (2.5 cm) of rain falls on 1 acre of land? What do raindrops look like?Let me introduce myself - I am Drippy, the (un) official USGS water-science icon. It is obvious that I am a raindrop, right? After all, all of you know that raindrops are shaped, well ... like me. As proof, you've probably seen me on television, in magazines, and in artists' representations. Truth is, I am "Drippy" and actually I am shaped more like a drip falling from a water faucet than a raindrop. The common raindrop is actually shaped more like a hamburger bun. As Alistair Frasier explains in his web page, Bad Rain, small raindrops, those with a radius of less than 1 millimeter (mm), are spherical, like a round ball. As droplets collide and grow in size, the bottom of the drop begins to be affected by the resistance of the air it is falling through. The bottom of the drop starts to flatten out until at about 2-3 mm in diameter the bottom is quite flat with an indention in the middle - much like a hamburger bun. Raindrops don't stop growing at 3 millimeters, though, and when they reach about 4-5 mm, things really fall apart. At this size, the indentation in the bottom greatly expands forming something like a parachute. The parachute doesn't last long, though, and the large drop breaks up into smaller drops. Precipitation rates vary geographically and over time Precipitation does not fall in the same amounts throughout the world, in a country, or even in a city. Here in Georgia, USA, it rains fairly evenly all during the year, around 40-50 inches (102-127 centimeters (cm)) per year. Summer thunderstorms may deliver an inch or more of rain on one suburb while leaving another area dry a few miles away. But, the rain amount that Georgia gets in one month is often more than Las Vegas, Nevada observes all year. The world's record for average-annual rainfall belongs to Mt. Waialeale, Hawaii, where it averages about 450 inches (1,140 cm) per year. A remarkable 642 inches (1,630 cm) was reported there during one twelve-month period (that's almost 2 inches (5 cm) every day!). Is this the world record for the most rain in a year? No, that was recorded at Cherrapunji, India, where it rained 905 inches (2,300 cm) in 1861. Contrast those excessive precipitation amounts to Arica, Chile, where no rain fell for 14 years, and in Bagdad, California, where precipitation was absent for 767 consecutive days from October 1912 to November 1914. The map below shows average annual precipitation, in millimeters and inches, for the world. The light green areas can be considered "deserts". You might expect the Sahara area in Africa to be a desert, but did you think that much of Greenland and Antarctica are deserts? On average, the 48 continental United States receives enough precipitation in one year to cover the land to a depth of 30 inches (0.76 meters). Precipitation size and speed Have you ever watched a raindrop hit the ground during a large rainstorm and wondered how big the drop is and how fast it is falling? Or maybe you've wondered how small fog particles are and how they manage to float in the air. The table below shows the size, velocity of fall, and the density of particles (number of drops per square foot/square meter of air) for various types of precipitation, from fog to a cloudburst. | | Intensity inches/hour (cm/hour) | Median diameter (millimeters) | Velocity of fall feet/second (meters/second) | Drops per second per square foot (square meter) | Fog | 0.005 (0.013) | 0.01 | 0.01 (0.003) | 6,264,000 (67,425,000) | Mist | .002 (0.005) | .1 | .7 (.21) | 2,510 (27,000) | Drizzle | .01 (0.025) | .96 | 13.5 (4.1) | 14 (151) | Light rain | .04 (0.10) | 1.24 | 15.7 (4.8) | 26 (280) | Moderate rain | .15 (0.38) | 1.60 | 18.7 (5.7) | 46 (495) | Heavy rain | .60 (1.52) | 2.05 | 22.0 (6.7) | 46 (495) | Excessive rain | 1.60 (4.06) | 2.40 | 24.0 (7.3) | 76 (818) | Cloudburst | 4.00 (10.2) | 2.85 | 25.9 (7.9) | 113 (1,220) | Source: Lull, H.W., 1959, Soil Compaction on Forest and Range Lands, U.S. Dept. of Agriculture, Forestry Service, Misc. Publication No.768 | | | Sources and more information Choose a water-cycle topic | A - Storage in ice and snow B - Precipitation C - Snowmelt runoff to streams D - Infiltration E - Groundwater discharge F - Groundwater storage G - Water storage in oceans H - Evaporation | I - Condensation J - Water storage in the atmosphere K - Evapotranspiration L - Surface runoff M - Streamflow N - Springs O - Freshwater storage P - Sublimation | | | | | Sponsor Advertisement BOOST Inverter Air Conditioner: | | BOOST DC Inverter Air Conditioner 16 SEER BOOST Inverter Air Conditioners meet our Highest Quality Featured, Energy Efficient, Environmentally Friendly, Certified Inverter Air Conditioners, manufactured with the highest standards for the United States, and Worldwide Markets; making them leaders in the dc inverter air conditioner industry. 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