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  2. Polar climate - Wikipedia

    en.wikipedia.org/wiki/Polar_climate

    A tundra climate is characterized by having at least one month whose average temperature is above 0 °C (32 °F), while an ice cap climate has no months averaging above 0 °C (32 °F). [2] In a tundra climate, even coniferous trees cannot grow, but other specialized plants such as the arctic poppy can grow. In an ice cap climate, no plants can ...

  3. Tree line - Wikipedia

    en.wikipedia.org/wiki/Tree_line

    The tree line follows the line where the seasonal mean temperature is approximately 6 °C or 43 °F. [12] [6] The seasonal mean temperature is taken over all days whose mean temperature is above 0.9 °C (33.6 °F). A growing season of 94 days above that temperature is required for tree growth. [13]

  4. Growing degree-day - Wikipedia

    en.wikipedia.org/wiki/Growing_degree-day

    Growing degrees (GDs) is defined as the number of temperature degrees above a certain threshold base temperature, which varies among crop species. The base temperature is that temperature below which plant growth is zero. GDs are calculated each day as maximum temperature plus the minimum temperature divided by 2, minus the base temperature.

  5. Polar forests of the Cretaceous - Wikipedia

    en.wikipedia.org/wiki/Polar_forests_of_the...

    According to experimental results, tree species with long lived evergreen foliage tend to benefit the greatest in a carbon dioxide rich environment because of their longer growing season and adaptations like canopy development that allow them to thrive in the temperate polar paleolatitudes of the Cretaceous. [4]

  6. Chilling requirement - Wikipedia

    en.wikipedia.org/wiki/Chilling_requirement

    The chilling requirement of a fruit is the minimum period of cold weather after which a fruit-bearing tree will blossom productively. It is often expressed in chill hours, which can be calculated in different ways, all of which essentially involve adding up the total amount of time in a winter spent at certain temperatures.

  7. Effect of Sun angle on climate - Wikipedia

    en.wikipedia.org/wiki/Effect_of_Sun_angle_on_climate

    At fixed latitude, the size of the seasonal difference in sun angle (and thus the seasonal temperature variation) is equal to double the Earth's axial tilt. For example, with an axial tilt is 23°, and at a latitude of 45°, then the summer's peak sun angle is 68° (giving sin(68°) = 93% insolation at the surface), while winter's least sun ...

  8. Scientists say Earth on track for disastrous sea level rise - AOL

    www.aol.com/news/2-degrees-40-feet-scientists...

    The report says if global average temperatures settle at 2 degrees Celsius above the preindustrial baseline, the planet could be committed to more than 40 feet of sea-level rise — a melt that ...

  9. Gravitropism - Wikipedia

    en.wikipedia.org/wiki/Gravitropism

    The actual optimal angle is a multi-parameter function, depending on time, the current reorientation angle and from the distance to the base of the fungi. The mathematical model , written following this suggestion, can simulate bending from the horizontal into vertical position but fails to imitate realistic behavior when bending from the ...