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Physical
Water cycle
River regimes
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Created by
Jenny
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Cards (9)
The
yukon
=
flows
thro
Alaska
climate
Conditions =
highly variable
across the
seasons
,
winter
= nearly
polar summer
=
high temp
flows
thro
diff types
of
climate inc tundra
and
mountain
the yukon
seasonality
winter= precipitation frozen= low flow
summer= precipitation does not
freeze
and
snowmelt
of winters precipit at ion=
high flow
the yukon
human influence
highly
natural landscape
= v
little human influence
on
river flow
the
amazon
climate
flows thro
tropical climate
relatively consistant
high temp Abada rate
of
precipitation
there is some
seasonal precipitation-
>
lower river discharge
high temp
and
high biodiversity-
>
high level
of
evapotranspiration
The
amazon
seasonality
consistent
temp
and
rainfall
create largely
consistent river flow
lower rainfall sept
and December->
lower river flow
La Niño years
=
chances
in
rainfall
= affect
river discharge levels
the
amazon
human influences
deforestation
affects
interception
,
infiltration
and
surface runoff
increasing the
flow
large dams
used by
Brazilian cities
for both
hydroelectric power
and
irrigation
= more
discharge
above
dam
and
reduced flow
below
dam
Murray-Darling
Australia
climate
seasonal sub tropic
basin
is in a
rain shadow
, surrounded by
mountains
collecting most of
regions rain
, causing periods of
prolonged drought
tribuataries north exp monsoon
,
tributaries south exp temperate climate
wet
(
aug-nov
) and
dry
(
jan-apr
) seasons causing
high
and
low river flows
Murray-Darling
seasonality
high seasonal variability
bc of
wet
and
dry seasons
impacted
by
changes
in
rainfall patterns
during
La Niña
and
El Niño yeard
La niña =
cooler sea temp
and
wet weather
el Niña =
opposite
and
less rainfall
Murray darling
human influence
water
is
drawn
from
Murray daring
for use in
cities
and to
irrigate farms
natural flow paths
of
river
have been
altered
for
human access-
>
loft
of
habitat
for
local animals
and
decline
in
water quality