soil moisture surplus - evapoT < precipitation - soil moisture store is full from the recharge period
soil moisture deficit - the only evapoT that occurs is the evapoT on precipitation - the soil moisture store has been exhausted
soil moisture utilisation - evapoT > precipitation - water used from soil moisture to meet demand - water not being replenished - losing more water than gaining
soil moisture recharge - precipitation > evapoT - gaining water - excess water recharges the soil moisture store
antecedent conditions - moisture that was already present in soil prior to rain
ablation
avalanches
meltwater
wind deposition
short term meteorological conditions can cause short term changes in the mass balance of a glacier i.e., seasonality
natural climate change cycles e.g., Milankovitch and sunspot cycles can impact mass balance overtime
climate change has a destabilising impact on mass balance because there is a positive feedback cycle
impacts can be linked to the hazard
profile
high areal extent can cause larger greater impacts
e.g., Afghanistan
2 people died in the
Paso Robles Quake
there is an interaction of physical factors and
the context surrounding the quake e.g., level of development
260 people died in the
Afghanistan-Pakistan EQ
Spatial predictability can also be a vital factor as areas with blind faults (such as Kobe 1995) can lead to
to increased risks due to a lack of understanding of the magnitude of the risk.
the significance of context in influencing the scale of disaster.
the level of development impacts effective management because
strategies that have seen more success are more expensive
2023 Japan appointed X to disaster prevention budget
$7bn - 1.2 trillion yen
high magnitude events are hard to manage
because they are infrequent
events in the pacific ocean have seen effective management because
they have high frequency which has enabled the effective use and modelling of the PWC prediction system in Hawaii
PTWC is used for
predicting tsunamis
Hawaii is monitored
24/7 by the PTWC
in geographically isolated areas it is hard to
receive aid e.g., Philippines has over 7000 islands
Earthquake in the Hindu Kush region did not receive much
aid in 2015 because it was in a remote location - over 300 people died + destruction to homes
scree is formed by
freeze thaw and weathering
scree is also formed by the disintegration of
exposed rock on the summit of mountains
a lip is formed at the bottom of the corrie
the glacier loses some erosive power and there is some deposition
erosional features formed to due ice sheet scouring
roche mountee
knock and lochan
crag and tail
ribbon lakes may be dammed by
a rock bar due to moraine at the edge of the lake
Different approaches may be needed to manage glaciate landscapes
environmental sensitivity of the area - SSSI?
differences in cultural value
may be a multiple economic use zone
differences in scale
different threats
different players
What percentage of movement is basal slip responsible for in warm glaciers
75%
glaciers near the sea will see accelerated rate of movement due to
positive feedback cycles
glacial movement can vary temporally
short term - seasons
long term - natural climate variations
local conditions can impact the rate of movement
altitude
rock type
medial moraines are
surface expressions of debris within the ice
lowland depositional landscapes are formed e.g.,
ablation till
lodgement till
till plain (ground moraine)
ground moraine is
blanket of till
sediment that has slowly built up over time
drumlins deposit material
subglacially
what type of moraine occurs when debris is scooped up and pushed to the front
terminal
Evidence of eratics?
Yorkshire dales has limestone rock but has some rock types but has some rock types from Scandinavia