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  2. Tectonic–climatic interaction - Wikipedia

    en.wikipedia.org/wiki/Tectonic–climatic...

    The climate surrounding the volcano constrains the impact of the eruption. Models of eruptions that treat climatic variables as controls and hold eruption intensity constant predict particulate emissions, such as volcanic ash and other pyroclastic debris ejected into the atmosphere, in the tropics to reach higher altitudes than eruptions in ...

  3. Land surface effects on climate - Wikipedia

    en.wikipedia.org/.../Land_surface_effects_on_climate

    Land surface effects on climate are wide-ranging and vary by region. Deforestation and exploitation of natural landscapes play a significant role. Some of these environmental changes are similar to those caused by the effects of global warming .

  4. Earth system interactions across mountain belts - Wikipedia

    en.wikipedia.org/wiki/Earth_system_interactions...

    Impacts on biotic processes have been investigated through phylogenetic analysis (by estimation of speciation and extinction rates) of mountain-adapted species (e.g. terrestrial tetrapods including amphibians, birds, and mammals [1] and butterflies [11] [47]) across mountain belts through time (e.g., [47]) and numerical diversification models ...

  5. Altitudinal zonation - Wikipedia

    en.wikipedia.org/wiki/Altitudinal_zonation

    Montane level: [7] [22] Extends from the mid-elevation forests to the tree line. The exact level of the tree line varies with local climate, but typically the tree line is found where mean monthly soil temperatures never exceed 10.0 degrees C and the mean annual soil temperatures are around 6.7 degrees C.

  6. Tectonic uplift - Wikipedia

    en.wikipedia.org/wiki/Tectonic_uplift

    Displacement of the Earth's surface with respect to the geoid. This is what we refer to as "surface uplift"; and surface uplift can be defined by averaging elevation and changes in elevation over surface areas of a specified size. The "uplift of rocks" refers to the displacement of rocks with respect to the geoid.

  7. Lapse rate - Wikipedia

    en.wikipedia.org/wiki/Lapse_rate

    At Earth's surface, the Tolman gradient would be about = (m), where is the temperature of the gas at the elevation of Earth's surface. Santiago and Visser remark that "gravity is the only force capable of creating temperature gradients in thermal equilibrium states without violating the laws of thermodynamics" and "the existence of Tolman's ...

  8. Elevational diversity gradient - Wikipedia

    en.wikipedia.org/wiki/Elevational_Diversity_Gradient

    The first recorded observation of the elevational diversity gradient was by Carl Linnaeus in his treatise On the growth of the habitable Earth. In this document, Linnaeus based his predictions on flood geology, assuming most of the world was at one point inundated, leaving only the highest elevations available for terrestrial life. Since, by ...

  9. Effects of climate change on biomes - Wikipedia

    en.wikipedia.org/wiki/Effects_of_climate_change...

    Climate change has a direct impact on the productivity of the boreal forest, as well as health and regeneration. [15] As a result of the rapidly changing climate, trees show declines in growth at the southern limit of their range, [ 61 ] and are migrating to higher latitudes and altitudes (northward) to remain their climatic habitat, but some ...