Systems Flashcards
Systems, physical factors and glacial movement
What is a system?
Set of interrelated objects comprising of components (STORES) and processes (LINKS) that are connected to work as a unified whole.
What type of system are glaciers?
Open systems - energy and matter can be transferred in as INPUTS and can also transfer OUTPUTS
Define negative feedback
A response to nullify the initial change
Define positive feedback
A response to amplify the initial change
Define glacial mass balance/budget
The difference between accumulation and ablation occurring over a one year time period.
Accumulation - ablation= annual budget
Define aeolian processes
CLIMATE
The process of wind carrying out erosion, transportation and deposition, acting on fine material
what are the varying rates of precipitation globally? (2 locations)
CLIMATE
HIGH LATITUDE Vostock station in Antarctica - 4.5mm /year
HIGH ALTITUDE Canadian Rockies - >600mm /year
what are the seasonal precipitation rates in Antarctica and the Canadian Rockies?
CLIMATE
Antarctica - less seasonal difference
Canadian Rockies - very varied seasonally: January 25mm, June 100mm
What is the effect of seasonal precipitation variation on the glacial budget?
CLIMATE
The more seasonally varied precipitation, the more varied the glacial budget
Why are glaciers in polar regions so thick despite low precipitation inputs?
CLIMATE
In high latitude locations, temps may never rise above 0c so no melting.
Define lithology
GEOLOGY
the physical and chemical composition of rocks.
2 examples of rocks with weak lithology
GEOLOGY
CLAY as the bonds within the rock are weak so little resistance to erosion, weathering and mass movements.
LIMESTONE made of calcium carbonate which is soluble to weak acids so its vulnerable to decay
by weathering through carbonation
Example of a rock with strong lithology
GEOLOGY
BASALT as its made of interlocking crystals, resistant to weathering its more likely to form landforms like aretes and pyramidal peaks
Define Structure
GEOLOGY
the properties of individual rock types such as jointing, bedding, faulting and permeability.
Examples with weak structure
GEOLOGY
CHALK is porous
CARBONIFEROUS LIMESTONE is highly jointed