Term 2 - Theme 3 (1) Flashcards
Observed sea level has increased around
10cm since 1970s.
Glaciers are driven by climate
Snow and ice accumulation, ablation through radiative forcing.
IPCC, 2001 + 2007
glaciers re the clearest indicators of what is currently happening to the climate of the earth… the fact that they are thinning and retreating at historically unprecedented rates should be a concern to us all.
Mass balance equation
MB = accumulation - ablation (-iceberg calving)
The cryosphere consists of
Northern hemisphere - Greenland, Arctic glaciers, Alaska, alps, himalayas (7m potential SLR).
Southern hemisphere - Antarctica - 57m potential SLR and the andes.
Change in glacier length
indirect, delayed sign of change in climate
Air temperature role
Related to radiation balance and solid/liquid precipitation ratio.
Climatic sensitivity of a glacier depends on
local topographic effects.
Response/lag time
Occur because the signal must be transferred from accumulation area to the snout of the glacier.
Response/lag time controlled by
glacier size, gradient and flow velocity. Lay, low gradient, slow glaciers will have a long lag time. Short, steep and fast glaciers will have a short lag time.
Monitoring frontal variations of glaciers
Direct measurement, image comparison.
Mass balance measurement of glaciers
Direct measurements of accumulation and ablation, remote sensing methods.
Global glacier changes (length)
General glacier recession shown in Little Ice Age. Intermittent readvances on decadal timescales. Strong glacier retreat in the 1920s and 1940s.
Glacier frontal variations
Most visible component of glacier response to climate change. May be studied over long time scales. All related to changes in total glacier mass balance.
global glacier change (mass balance)
mass balance is the different between mass gained and mass lost. Mountain glaciers are losing mass all the time + this has increased in the last decade.