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  2. Humidity - Wikipedia

    en.wikipedia.org/wiki/Humidity

    Humidity is the concentration of water vapor present in the air. Water vapor, ... Environmental humidity is affected by winds and by rainfall.

  3. Museum environments - Wikipedia

    en.wikipedia.org/wiki/Museum_environments

    Garry Thomson's 1978 publication The Museum Environment [12] was a major influence in the development of environmental guidelines for cultural organisations and the field of preventive conservation. Though critical analysis shows that Thompson did not intend for his recommended parameters for temperature and relative humidity to become 'rules ...

  4. Tropical climate - Wikipedia

    en.wikipedia.org/wiki/Tropical_climate

    Depending on the location of the region, the wet and dry seasons can have varying duration. Annual temperature changes in the tropics are small. Due to the high temperatures and abundant rainfall, much of the plant life grows throughout the year. High temperature and humidity is the most suitable environment for epiphytes to grow. [5]

  5. Damp (structural) - Wikipedia

    en.wikipedia.org/wiki/Damp_(structural)

    Humidity occurs in indoor environments due to building related causes. Porous walls, rising damp, and leaks in the building are determinants for structural dampness due to elevated humidity levels. [4]: 185–187 The construction of the building can also lead to humidity and unwanted moisture in the indoor environment. [15]

  6. Humid continental climate - Wikipedia

    en.wikipedia.org/wiki/Humid_continental_climate

    The snowy city of Sapporo, Japan, has a humid continental climate (Köppen Dfa).. Using the Köppen climate classification, a climate is classified as humid continental when the temperature of the coldest month is below 0 °C [32.0 °F] or −3 °C [26.6 °F] and there must be at least four months whose mean temperatures are at or above 10 °C (50 °F). [5]

  7. Environmental gradient - Wikipedia

    en.wikipedia.org/wiki/Environmental_gradient

    An environmental gradient, or climate gradient, is a change in abiotic (non-living) factors through space (or time). Environmental gradients can be related to factors such as altitude, depth, temperature, soil humidity and precipitation.