The climate of Sapa is highly seasonal, with a subtropical
climate in the summer and a temperate climate during the winter. Average
temperature for Sapa town is 15.4ºC, with a maximum of 29.4ºC and a
minimum of 1ºC.
Sapa , is a frontier town and capital
of Sa Pa District in the Lao Cai province in northwest Vietnam. It is
one of the main market towns in the area, where several ethnic minority
groups such as Hmong, Dao (Yao), Giay, Pho Lu, and Tay live.
For
the most pleasant weather, the best times to visit Sapa is March and
May or mid-September to early December. While trips can be enjoyed
year-round, the winters in Sapa get cold, with some fog and drizzle, and
the summers have the hottest weather and higher chances of rain, with
the rainy season starting in May through September.
The
Hoang Lien Mountains are home to a rich variety of plants, birds,
mammals, amphibians, reptiles and insects, many only found in
northwestern Vietnam. For this reason, the Hoang Lien Nature Reserve was
made a National Park in 2006, and covers much of the mountain range to
the immediate south of Sa Pa.
Forest type and quality change with
increasing altitude. At 2000 meters the natural, undisturbed forest
begins to be seen. Above 2500 meters dwarf conifers and rhododendrons
predominate in the harsh “elfin forest”, so called because a lack of
topsoil and nutrients means that fully mature trees grow to measure only
a few meters in height. Higher still, only the hardiest of plant
species are found. At over 3000 meters, Fan Si Pan’s summit can only
support dwarf bamboo.
The climate of Hoang Lien National Park is
unique to Vietnam. It is highly seasonal, with a subtropical climate in
the summer and a temperate climate during the winter. Mean annual
temperature for Sa Pa town is 15.4°C, with a maximum of 29.4°C and a
minimum of 1°C. The warmest months are July and August, and the coldest
months are December and January. Snow falls in some years on the highest
peaks.
Climate
varies considerably within the national park. The prevalent wind
direction for most of the year is west to east, leading to cloud
formation on the upper slopes of the Fansipan massif. These
high-altitude areas are covered by cloud most days of the year and have
very high humidity. Cloud also penetrates into the valleys but these
areas are usually less humid than the mountain slopes. In the extreme
east of the national park, around Ban Ho village, mean temperatures are
considerably higher due to the lower altitude of these areas.
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