Difficulties in monitoring and predicting climate change include, timescales, spatial scales, interconnected systems, natural fluctuations and time delay between cause and affect
The slowing of the North Atlantic gulf decreases temperatures lining Coast this is an example of an interconnected system
Data collection for climate change may include monitoring ocean currents. Computer models, ice core data, satellite data and other
We can use satellites to measure, wind velocity, ocean currents, wave height and vegetation cover
Timescales make monitoring and predicting difficult, for instance shirt term time scale can involve sudden storm or wet winters or long term can involve a trend of winters with increasing rainfall
Spatial scales can be local, rehional or global
Spatial scales locally can involve sudden but slow moving storm causing flooding locally, globally may involve increasing global temperatures due to uv absorbtion
Intercomnected systems make it difficult, e.g. chnage in jetstreams may cause temperature rise, or slowing of North Atlantic may cause temperature decrease
Natural fluctuations make it difficult because all climatic factors fluctuate because they are influenced by variability in solar outpuy
Time delay between cause and affect makes it difficult