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The Mpemba effect is the name given to the observation that a liquid (typically water) that is initially hot can freeze faster than the same liquid which begins cold, under otherwise similar conditions. There is disagreement about its theoretical basis and the parameters required to produce the effect. [1] [2]
Science Buddies mission is to help students to build their literacy in science and technology so they can become productive and engaged citizens in the 21st century. The site has personalized learning tools, over 15,000 pages of scientist-developed subject matter (including experiments based on the latest academic research), and an online ...
The Wegener–Bergeron–Findeisen process (after Alfred Wegener, Tor Bergeron and Walter Findeisen []), (or "cold-rain process") is a process of ice crystal growth that occurs in mixed phase clouds (containing a mixture of supercooled water and ice) in regions where the ambient vapor pressure falls between the saturation vapor pressure over water and the lower saturation vapor pressure over ice.
A New Jersey doctor thinks he might have the next miracle trick to melt away those stubborn pounds - literally. Dr. Brian Weiner, a gastroenterologist, says his Ice Diet will help you burn more ...
Different stages of ice melt in a pond The melting of floating ice. Ablation of ice refers to both its melting and its dissolution. [103] The melting of ice entails the breaking of hydrogen bonds between the water molecules. The ordering of the molecules in the solid breaks down to a less ordered state and the solid melts to become a liquid.
' study of ice ') is the scientific study of glaciers, or, more generally, ice and natural phenomena that involve ice. Glaciology is an interdisciplinary Earth science that integrates geophysics , geology , physical geography , geomorphology , climatology , meteorology , hydrology , biology , and ecology .
Examples of tipping points include thawing permafrost, which will release methane, a powerful greenhouse gas, or melting ice sheets and glaciers reducing Earth's albedo, which would warm the planet faster. Thawing permafrost is a threat multiplier because it holds roughly twice as much carbon as the amount currently circulating in the atmosphere.
It normally is a Type I gas clathrate. [2] There has also been some experimental evidence for the development of a metastable Type II phase at a temperature near the ice melting point. [1] [3] [4] The clathrate can exist below 283K (10 °C) at a range of pressures of carbon dioxide.