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atmosphere: CO2 Concentration


390 360 330 300 270


320 300 280 260


atmosphere: N2O Concentration


1800 1600 1400 1200 1000 800 600


atmosphere: CH4 Concentration


atmosphere: Antarctic ozone depletion 1.0


60 40 20 0


0.4 0


-0.6


climate:


Northern hemisphere average surface temperature


0.04 0.03 0.02 0.01 0


climate: Great floods


100 80 60 40 20 0


ocean ecosystems: Disappearing fish stocks


4 3 2 1


0


coastal zone: Alteration


10 8 6 4 2 0


coastal zone: Biogeochemistry


terrestrial ecosystems: Loss of tropical rain forest and woodland


30 20 10 0


50% 25% 0


terrestrial ecosystems: Amount of domesticated land


30 20 10 0


global biodiversity: Rate of species loss


Figure 1.1 Humanity’s remarkable environmental journey from the industrial revolution until today. Starting in the mid-1950s, we see for the fi rst time, global-scale changes in Earth system in essentially all of the environmental processes that form the basis for our modern economy. Why? Due to the dramatic increase in human activity.


28


THE HUMAN QU EST – PROSP E R ITY WITH IN PLAN ETARY BO U N DAR I ES


% of 1700 value


% Fisheries fully exploited


% Loss of total column ozone


CO2 (ppmv)


% of Total land area


Shirmp farm production Million MT


Temperature Anomaly (°C)


N2O (ppbv)


Species extinctions (thousand)


(1012 moles/year) Nitrogen Flux


Decadal flood frequency


CH4 (ppbv)


year 1750 1800 1850 1900 1950 2000 year 1750 1800 1850 1900 1950 2000 year 1750 1800 1850 1900 1950 2000 year 1750 1800 1850 1900 1950 2000 year 1750 1800 1850 1900 1950 2000 year 1750 1800 1850 1900 1950 2000 year 1750 1800 1850 1900 1950 2000 year 1750 1800 1850 1900 1950 2000 year 1750 1800 1850 1900 1950 2000 year 1750 1800 1850 1900 1950 2000 year 1750 1800 1850 1900 1950 2000 year 1750 1800 1850 1900 1950 2000


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