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  2. Climate change in Nepal - Wikipedia

    en.wikipedia.org/wiki/Climate_change_in_Nepal

    Köppen climate classification map for Nepal for 1980–2016. ... which has high intensity rainfall during rainy season. It has resulted in heavy floods, ...

  3. File:Nepal map of Köppen climate classification.svg - Wikipedia

    en.wikipedia.org/wiki/File:Nepal_map_of_Köppen...

    You are free: to share – to copy, distribute and transmit the work; to remix – to adapt the work; Under the following conditions: attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made.

  4. Geography of Nepal - Wikipedia

    en.wikipedia.org/wiki/Geography_of_Nepal

    A land cover map of Nepal using Landsat 30 m (2010) data. ICIMOD ’s first and most complete national land cover [ 24 ] database of Nepal prepared using public domain Landsat TM data of 2010 shows that show that forest is the dominant form of land cover in Nepal covering 57,538 km 2 with a contribution of 39.09% to the total geographical area ...

  5. Köppen climate classification - Wikipedia

    en.wikipedia.org/wiki/Köppen_climate_classification

    The length and severity of the dry season diminish inland (southward); at the latitude of the Amazon River—which flows eastward, just south of the equatorial line—the climate is Af. East from the Andes , between the dry, arid Caribbean and the ever-wet Amazon are the Orinoco River's Llanos or savannas , from where this climate takes its name.

  6. Inner Terai Valleys of Nepal - Wikipedia

    en.wikipedia.org/wiki/Inner_Terai_Valleys_of_Nepal

    Nepal topography. The green/yellow zones hold the Inner Terai valleys. The Terai has a humid, subtropical climate. The mean annual rainfall at the Rampur weatherstation in Chitwan was 2,214 mm (87.2 in) between 1995 and 2006. More than 80% of the total annual rainfall occurs during the monsoon season from June to September. Average temperatures ...

  7. Monsoon of South Asia - Wikipedia

    en.wikipedia.org/wiki/Monsoon_of_South_Asia

    Over India, a subtropical westerly jet develops in the winter season and is replaced by the tropical easterly jet in the summer season. The high temperature during the summer over the Tibetan Plateau, as well as over Central Asia in general, is believed to be the critical factor leading to the formation of the tropical easterly jet over India.

  8. Monsoon - Wikipedia

    en.wikipedia.org/wiki/Monsoon

    The rainy season occurs from September to February and it is a major source of energy for the Hadley circulation during boreal winter. It is associated with the development of the Siberian High and the movement of the heating maxima from the Northern Hemisphere to the Southern Hemisphere.

  9. Nepalgunj - Wikipedia

    en.wikipedia.org/wiki/Nepalgunj

    Nepalgunj has a sub-tropical climate. Temperatures sometimes exceed 40 °C (104 °F) from April to June. During the rainy season—arriving in June and lasting into September—it is less hot but sometimes very humid. Winter is usually pleasant while the sun is out.