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Kilimanjaro towers an
incredible 5,000m above its surrounding
plains and is so big it has its own weather patterns. In theory
there are 4 annual seasons: 2 wet and 2 dry. In simple terms these
are caused by various battles
between the moist south easterly Trade Winds blowing from the Indian
Ocean, the dry Anti-trade Winds coming in from the north east and
later in the year the remnants of the north easterly monsoon.
From
March to May and again from November to February the moist winds
prevail and deposit varying amounts of precipitation on the southern
and northern flanks of the mountain respectively. The other months are the dry
seasons, with the period from June to October, during which we will
be climbing
the mountain, being both the driest and coldest months of the year,
given that Kilimanjaro lies south of the equator and experiences its winter during the northern hemisphere summer. Indeed, August when we are intending to
be camping out, is one of the coldest months of the year!
That,
at least,
is the theory but anyone who has been in the mountains knows that
things are seldom so simple, so the reality is probably far less
predictable. We'll just have to wait and see what the mountain
actually throws at us.
The
other feature of climbing Kilimanjaro is that one effectively
experiences every type of weather from equatorial rain forest to
arctic ice within a week and all that while sleeping under canvas.
Once they leave Moshi or
Arusha the climber traverses 5 climatic zones before they reach the summit,
each with its own flora and fauna. What follows is a
brief resume of what we can expect but we'll add photos and more
about our experience upon our return.
The Cultivation Zone from 800m to 1,800m
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Below the
rain forest, this zone offers fertile land for habitation
and cultivation. It marks the zone through which the climber
travels en-route to the Kilimanjaro National Park and the
climb itself. The days here are hot, though night time
temperatures can be cool to cold and there are frequent
short rain showers that keep the fertile soil moist and
facilitate the growing of crops like coffee, bananas, mangos
as well as crops like beans and cabbage more common to
visitors from Europe or the USA. |
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The Montane Rain Forest from 1,800m to 2,800m
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The most important zone for man and
animals as the forest, together with run-off from the glaciers, is
the region's main source of water as well as home to some 80% of the
area's flora and fauna. Wood from the forest finds innumerable uses
from carpentry to burning and the forest is home to more than 1,000
species of plants. It starts at the same altitude as most routes and
throughout its 1,000 metres experiences significant daily
precipitation.
Indeed, the annual average is
a whopping 2.3m of rainfall, or, to put it another way,
enough water to fill the average ground floor of UK houses
right up to the ceiling! The
flora here includes camphor woods, fig, giant ferns and old man's
beard draped from most of the branches. Towards its upper limit
giant heathers begin to appear and can grow to ten metres high.
This
is where one is most likely to see significant
wildlife. This could include blue monkeys, baboons, or
leopard, though sightings are very rare, We heard monkeys of some
kind but saw nothing.
Temperatures are commonly
in the twenties to thirties and it is the need to pass
through this rather damp zone that necessitates the climber ensuring all equipment is packed in water-tight bags
and that waterproofs are in the daypack.
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Heath and Moorland from 2,800m to 4,000,
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Thinning forest, smaller and smaller trees and an ever-increasing
abundance of giant heather are the sign that one is moving above the
rain forest and into the Heath and Moorland zone, also known as the
Low Alpine zone. However, the higher one climbs the less giant the heathers
become, though they can still reach 3m. There is also an abundance
of everlasting flowers as one moves higher
In the upper reaches
of the zone, in the moorlands, the climber begins to come into contact
with the most distinctive plant on the mountain - the Senecio. There
are two types of Senecio on Kili. One grows at altitudes between 2,500m and
4,000m and can be up to 5m tall and the other grows only above
3,600m. There are a lot around Barranco Camp. In terms of animals, there are
small "four-striped" mice but little else at these altitudes.
This is a misty place, which combines with the strange vegetation to
make it feel like Jurassic Park. As one moves higher this gives
way to Alpine Heath characterised by bushes, grasses and shrubs. One may encounter the
odd heavy shower but the mist provides most of the precipitation.
Even so, annual precipitation is still 1.3m decreasing to only 500mm or so in the upper
moorland areas. Temperatures can be as high as 30 degrees during the day, plummeting
to below freezing at night.
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The Alpine Desert from 4,000m to 5,000m
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Above
about 4,000m most of the vegetation has disappeared leaving a bare,
stony, desert-like landscape with only a few grasses and alpines to
dot the landscape. The zone is very dry with annual precipitation
only about 200mm and is dominated by temperatures between zero and
minus ten degrees and by cold winds that whip up the dust into mini
sandstorms. Sporadic rain is also possible. At night it
is bitterly cold with temperatures falling well below freezing. The
habitat provides neither protection nor food for animal life,
meaning that apart from a few insects, spiders and mice it is devoid
of animals, making it even bleaker for those trekking slowly though
it.
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The Ice Cap Zone from 5,000m to 5,895m
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This is the most inhospitable zone. Virtually no water
and extremely bleak, grey and dismal with little
protection afforded to those who enter it. Snow, icy
winds and extreme falls in night temperatures are common. There
is virtually no vegetation and no
animals, though in 1926 a mummified
leopard was found at 5,700m on the crater rim and is marked on
maps as "Leopard Point".
The scenic highlights up here are the Reusch
Crater and the 15 glaciers
including Rebmann Glacier, pictured here, which was our companion as we pushed
for the summit through the freezing night air with temperatures as low as minus 25
degrees and a biting 120km per hour, or hurricane force 12, wind to buffet us as we climb
ever higher.
At these extremes wind chill becomes a
real issue with effective temperatures plummeting to as low as
minus 48 degrees Celsius. Even if the temperature was as high as
minus 15 degrees and the wind only Gale Force the wind chill
was below minus 30.
We don't know how cold it was
up there but suffice to say it was so cold that the video
camera could not fire up its hard disc and gave a message to
the effect that it was all too cold.
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Beaufort number |
Description |
Wind speed |
Conditions |
Wind chill
at -15/-20
Celsius |
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km/h |
mph |
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7 |
High wind, near gale |
50-61 |
31-38 |
Whole trees in motion. Effort
needed to walk against wind. Swaying of skyscrapers may be
felt. |
-29/-36 |
|
8 |
Gale |
62-74 |
39-46 |
Twigs break from trees. Cars
veer on road. Progress on foot seriously impeded. |
-30/-37 |
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9 |
Strong
gale |
75-88 |
47-54 |
Branches break, small trees blow
over. Construction/temporary signs and barricades blow over.
Damage to circus tents and canopies. |
-31/-38 |
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10 |
Storm, whole gale |
89-102 |
55-63 |
Trees broken off or uprooted,
saplings bent and deformed. Poorly attached asphalt shingles
peel off roofs. |
-32/-39 |
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11 |
Violent storm |
103-117 |
64-72 |
Widespread vegetation damage.
Many roofing surfaces damaged |
-33/-40 |
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12 |
Hurricane
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≥118 |
≥73 |
Very widespread damage to
vegetation. Windows may break; mobile homes and poorly
constructed sheds and barns damaged. Debris may be hurled
about. |
-34/-41 |
Based on this it looks as though we
can expect effective temperatures of somewhere between minus 30 and
minus 40 degrees on summit night, which is really quite nippy to say
the least!
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