in India with
Cwa climate
Subtropical monsoon climate A
Subtropical monsoon climate, officially classified as a
Subhumid subtropical climate or
Monsoon-influenced humid subtropical climate under the Köppen classification (
Cwa), has a hot summer. This climate is extensively present in
South and
Southeast Asia, mainly
North India,
Southern China,
Myanmar and
Nepal and
Southern Africa,
Zambia and
Angola; it can also be found in
South America, isolated zones of
Bolivia,
Brazil and
Argentina. It also occurs in parts of tropical highlands of
São Paulo state,
Mato Grosso do Sul and near the
Andean highland in northwestern
Argentina. These highland areas feature summer temperatures that are warm enough to fall outside the
subtropical highland climate category
Cwb.
Subtropical highland climate ,
Jalisco in the green, example of
Cwb climate with coniferous groves A
Highland subhumid temperate climate, officially classified as a
Subtropical highland climate or
Monsoon-influenced temperate oceanic climate under the Köppen classification (
Cwb), exists in elevated portions of the world that are within either the tropics or subtropics, though it is typically found in mountainous locations in some tropical countries. Despite the latitude, the higher altitudes of these regions mean that the climate tends to share characteristics with
oceanic climates.
Subpolar subhumid temperate climate A
Subpolar subhumid temperate climate, officially classified as a
Cold subtropical highland climate or
Monsoon-influenced subpolar oceanic climate under the Köppen classification (
Cwc), is a sub-alpine climate. It is located only in Andean high plains in Bolivia and Perú, from 3200 m until 4000 m. It is a transition climate between
Cwb and
alpine climate ET. ==See also==