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  2. Land surface effects on climate - Wikipedia

    en.wikipedia.org/.../Land_surface_effects_on_climate

    A rain shadow is a dry area on the leeward side of a mountainous area (away from the wind). The mountains block the passage of rain-producing weather systems and cast a "shadow" of dryness behind them. Wind and moist air are drawn by the prevailing winds towards the top of the mountains, condensing and precipitating before it crosses the top.

  3. Earth system interactions across mountain belts - Wikipedia

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

    Reconstructions of mountain belt paleotopography helps scientists understand the influence of mountain growth on climate and montane ecosystem biodiversity. [5] [35] [39] Paleotopography is commonly analysed using § Stable isotope paleoaltimetry (e.g., [5] [2]).

  4. Altitudinal zonation - Wikipedia

    en.wikipedia.org/wiki/Altitudinal_zonation

    Heating of solids, sunlight and shade in different altitudinal zones (Northern hemisphere) [5] A variety of environmental factors determines the boundaries of altitudinal zones found on mountains, ranging from direct effects of temperature and precipitation to indirect characteristics of the mountain itself, as well as biological interactions of the species.

  5. Kids and teens are feeling climate anxiety. Here's how ... - AOL

    www.aol.com/kids-teens-feeling-climate-anxiety...

    Youth are increasingly stressed about the state of the environment and climate change. Here are tips on how to help your child. Kids and teens are feeling climate anxiety.

  6. Tectonic–climatic interaction - Wikipedia

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

    Tectonic–climatic interaction is the interrelationship between tectonic processes and the climate system. The tectonic processes in question include orogenesis, volcanism, and erosion, while relevant climatic processes include atmospheric circulation, orographic lift, monsoon circulation and the rain shadow effect.

  7. Rain shadow - Wikipedia

    en.wikipedia.org/wiki/Rain_shadow

    The climate of the islands is tropical, and rainfall is brought by trade winds from the east. The western side of the Grande Terre lies in the rain shadow of the central mountains, and rainfall averages are significantly lower. On the South Island of New Zealand is found one of the most remarkable rain shadows anywhere on Earth.

  8. Mountain breeze and valley breeze - Wikipedia

    en.wikipedia.org/wiki/Mountain_breeze_and_valley...

    Mountain and valley breezes are other examples of local winds caused by an area's geography. Campers in mountainous areas may feel a warm afternoon quickly change into a cold night soon after the sun sets. During the day, the sun warms the air along the mountain slopes. This warm air rises up the mountain slopes, creating a valley breeze.

  9. Climate change and children - Wikipedia

    en.wikipedia.org/wiki/Climate_change_and_children

    Children often have no voice in terms of global responses to climate change. [5] People living in low-income countries experience a higher burden of disease and are less capable of coping with climate change-related threats. [7] Nearly every child in the world is at risk from climate change and pollution, while almost half are at extreme risk. [8]