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  2. Cold hardening - Wikipedia

    en.wikipedia.org/wiki/Cold_hardening

    Plant covered in snow after an ice storm in 2013, Ontario, Canada Rosa canina covered in frost, Swabian Jura. Plants in temperate and polar regions adapt to winter and sub zero temperatures by relocating nutrients from leaves and shoots to storage organs. [1]

  3. Snow hydrology - Wikipedia

    en.wikipedia.org/wiki/Snow_hydrology

    It is capable of detecting and categorizing snow cover into three zones for data calculations. The first zone is an area with 100% snow cover. The second zone is known as the transition zone, which is a mixture of snow covered regions and non snow covered regions. This zone is commonly measured at a 50% snow composition value.

  4. Subnivean climate - Wikipedia

    en.wikipedia.org/wiki/Subnivean_climate

    In winter regions that do not have permafrost, the subnivean zone maintains a temperature of close to 32 °F (0 °C) regardless of the temperature above the snow cover, once the snow cover has reached a depth of six inches (15 cm) or more. The sinuous tunnels left by these small mammals can be seen from above when the snow melts to the final ...

  5. 7 Tips For Bringing Outdoor Plants Inside For Winter - AOL

    www.aol.com/lifestyle/7-tips-bringing-outdoor...

    Ideally, isolate your outdoor plants from your indoor plants for 4 to 6 weeks when you first bring them inside. If that’s not practical, keep them away from other plants for about 1 to 2 weeks ...

  6. Winter rest - Wikipedia

    en.wikipedia.org/wiki/Winter_rest

    Winter rest (from the German term Winterruhe) is a state of reduced activity of plants and warm-blooded animals living in extratropical regions of the world during the more hostile environmental conditions of winter. In this state, they save energy during cold weather while they have limited access to food sources.

  7. Snow science - Wikipedia

    en.wikipedia.org/wiki/Snow_science

    Snow density (ρ s) is the mass per unit volume of snow of a known volume, calculated as kg/m 3. Classification runs from very fine at below 0.2 mm to very coarse (2.0–5.0 mm) and beyond. Snow hardness (R) is the resistance to penetration of an object into snow. Most snow studies use a fist or fingers for softer snows (very soft through ...

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    Get AOL Mail for FREE! Manage your email like never before with travel, photo & document views. Personalize your inbox with themes & tabs. You've Got Mail!

  9. Snowpack - Wikipedia

    en.wikipedia.org/wiki/Snowpack

    Snowpack is an accumulation of snow that compresses with time and melts seasonally, often at high elevation or high latitude. [1] [2] Snowpacks are an important water resource that feed streams and rivers as they melt, sometimes leading to flooding. Snowpacks provide water to down-slope communities for drinking and agriculture. [3]

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