{"id":11270,"date":"2024-02-19T10:00:00","date_gmt":"2024-02-19T10:00:00","guid":{"rendered":"https:\/\/modernsciences.org\/staging\/4414\/?p=11270"},"modified":"2024-02-08T17:37:46","modified_gmt":"2024-02-08T17:37:46","slug":"how-can-i-get-ice-off-my-car-an-engineer-who-studies-airborne-particles-shares-some-quick-and-easy-techniques","status":"publish","type":"post","link":"https:\/\/modernsciences.org\/staging\/4414\/how-can-i-get-ice-off-my-car-an-engineer-who-studies-airborne-particles-shares-some-quick-and-easy-techniques\/","title":{"rendered":"How can I get ice off my car? An engineer who studies airborne particles shares some quick and easy\u00a0techniques"},"content":{"rendered":"\n
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\n Condensation and cold combine to create that layer of ice on car windshields in winter.\n Tomasz Sienicki\/Wikimedia Commons<\/a>, CC BY-SA<\/a><\/span>\n <\/figcaption>\n <\/figure>\n\nSuresh Dhaniyala<\/a>, Clarkson University<\/a><\/em><\/span>\n\n

If you live somewhere that gets cold in the winter, you\u2019ve probably seen cars parked outdoors covered in a thin layer of ice on a chilly morning. But what causes this frost, and how can you get rid of it quickly?<\/p>\n\n

I\u2019m a mechanical engineering professor<\/a> who studies how water vapor interacts with airborne particles under different atmospheric conditions. Frosty windshields are similar to some of the thermodynamic questions I study in the lab, and they\u2019re also a pesky issue that I deal with every winter on my way to work. <\/p>\n\n

Windshield condensation<\/h2>\n\n

The air in Earth\u2019s atmosphere always contains a certain amount of water vapor, but there\u2019s only so much water vapor the air can hold. Scientists call that limit 100% relative humidity<\/a>. The dew point<\/a> refers to the temperature at which relative humidity reaches 100%. <\/p>\n\n

Wet air has high dew point temperature, while dry air has a low dew point temperature. With each degree drop in temperature, the air gets closer to its dew point temperature \u2013 or its water vapor carrying capacity. Any cooling after the dew point temperature has been reached causes water to condense onto surfaces<\/a>, or form into fog.<\/p>\n\n

Overnight, car windshields facing the cold dark sky are radiatively cooled<\/a>, meaning they release heat out into their surrounding area in the form of visible and invisible light. As air comes in contact with the cold windshield, it can reach its dew point temperature. Then, the water vapor condenses onto the windshield.<\/p>\n\n

When this radiative cooling drops the temperature on the windshield\u2019s surface to below the freezing point<\/a>, 32 degrees Fahrenheit (zero degrees Celsius), the layer of condensed water on the windshield turns to frost. <\/p>\n\n

Defrosting your car<\/h2>\n\n

To defrost an icy windshield, you can follow a few different approaches, some of which take longer and require more effort than others.<\/p>\n\n

One option is to directly spray a small amount of warm liquid on the layer of frost to help melt it. For this approach to work, the spray liquid must be hot enough to raise the overall temperature of the frost layer to above the melting point<\/a>. But the temperature can\u2019t be way hotter than the temperature of the glass or you\u2019ll crack your windshield. <\/p>\n\n

A better way to melt the ice without damaging your car is to spray your windows with a warm liquid that has a lower freezing point than water, like a mixture of rubbing alcohol and water. This warm mixture will melt the frost layer without heating up the glass, and the resulting liquid layer on the windshield will have a lower freezing point than water. It will remain liquid, and you can wipe it away with your windshield wipers. <\/p>\n\n

Similar alcohol and water mixtures \u2013 glycol, for example<\/a> \u2013 are commonly used to maintain the icy surface of skating rinks<\/a>.<\/p>\n\n

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