BIOLOGY, TOPIC FIVE,5, CLIMATE CHANGE Flashcards
EVIDENCE, FOR CLIMATE CHANGE.
SCIENTISTS CANNOT GO BACK IN TIME, TO DIRECTLY MEASURE CLIMATIC VARIBALES, SUCH AS AVERAGE TEMPERATURE AND PRECIPITATION, THEY MUST INSTEAD INDIRECTLY MEASURE TEMPERATURE.
EVIDENCE FOR CLIMATE CHANGE, ANTARTIC ICE CORES.
ANTARTIC ICE CORES, HAVE BEEN COLLECTED AND ANALYSED, TO INDIRECTLY ESTIMATE THE TEMPERATURE, OF EARTH OVER THE PAST 400,000 YEARS.
BY MEASURING THE AMOUNT OF CARBON DIOXIDE, CO2, TRAPPED IN THE ICE, SCIENTISTS HAVE DETERMINED, PAST ATMOSPHERIC CARBON DIOXIDE, CO2, CONCENTRATIONS.
THE ATMOSPHERIC CONCENTRATION OF CARBON DIOXIDE, CO2, HAS RISEN STEADILY SINCE THE BEGINING OF INDUSTRIALISATION.
DENDOCHRONOLOGY.
DENDOCHRONOLOGY, TREE RINGS, IS A METHOD TO ASCERTAIN THE RISE IN TEMPERATURE OF EARTH.
IT IS THE STUDY OF THE RINGS FORMED WITHIN THE TRUNKS.
EACH YEAR, A NEW RING IS FORMED WITHIN THE TRUNK.
THE NUMBER OF RINGS, EQUALS THE AGE OF THE TREE.
RECENT STUDIES SHOW, THAT THE THICKNESS OF THE RINGS FORMED IN THE 20TH CENTURY, ARE MORE THAN THOSE FORMED EARLIER.
THIS IS A CLEAR INDICATION OF A WARMER CLIMATE.
WHAT IS A PEAT BOG?
A PEAT BOG, IS A TYPE OF ACIDIC WETLAND, WHICH PRESERVES THE POLLEN LAYER-BY-LAYER AS TIME PASSES.
POLLEN IN A PEAT BOG.
POLLEN IN A PEAT BOG, IS ANOTHER METHOD FOR DETERMINING CLIMATE CHANGE.
POLLENS ARE OFTEN TRAPPED IN PEAT BOGS.
COLLECTING POLLEN GIVES INSIGHT INTO THE CLIMATE THAT WAS PREVELANT, WHEN THE POLLEN WAS TRAPPED.
CLIMATE CHNAGE, IMPACTS THE NATURE OF POLLEN, AND THE GRADUAL INCREASE IN THE TYPE OF POLLEN THAT THRIVE BETTER IN A WARMER CLIMATE, SHOWS A TREND OF INCREASING TEMPERATURE.
CLIMATE CHANGE, DUE TO HUMAN ACTIVITY.
HUMAN ACTIVITY RELEASES CARBON DIOXIDE, CO2, AND METHANE, CH4, TWO OF THE MOST SIGNIFICANT GREENHOUSE GASES, INTO THE ATMOSPHERE.
THE PRIMART MECHANISM THAT RELEASES CARBON DIOXIDE, CO2, IS THE BURNING OF FOSSIL FUELS, SUCH AS GASOLINE, COAL, AND NATUAL GAS.
THE EFFECTS OF CLIMATE CHANGE, THE MELTING OF POLAR ICE CAPS.
MELTING OF POLAR ICE CAPS, REDUCES SPECIES BIODIVERSITY, DESTROYS HABITATS AND SOME SPECOIES BECOME EXTINCT.
RISING SEA LEVELS FROM MELTING ICE CAPS, AND THERMAL EXPANSION OF OCEANS COULD FLOOD LOW-LYING LANDS, REDUCING TERRESTRIAL HABITATS, AND REDUCING FRESHWATER HABITATS AS SEAWATER MOVES UP RIVERS.
EFFECTS OF CLIMATE CHANGE, HIGH TEMPERATURES AND LESS RAINFALL.
HIGH TEMPERATURES AND LESS RAINFALL, XEROPHYTIC PLANTS WILL BECOME DOMINANT OTHER SPECIES WILL BE LOST ALONG WITH ANIMAL SPECIES THAT RELY ON THOSE PLANTS AS A FOOD SOURCE.
EFFECTS OF CLIMATE CHANGE, WARMER CLIMATES.
INSECTS ARE ADAPTED TO CERTAIN WARMER CLIMATES, BUT IF THERE IS A GLOBAL TEMPERATURE RISE, THE INSECTS CAN LIVE ANYWHERE, CARYY NEW PATHOGENS TOWARDS THE POLES, REDUCING SPECIES BIODIVERSITY, AS THEY CANOT FIGHT THE NEW DISEASESE.
INVESTIGATING THE EFFECT OF TEMPERATURE ON ENZYME ACTIVITY.
INCREASE IN TEMPERATURE, INCREASES KINETIC ENERGY.
SO MOR ENZYME SUBSTRATE COMPLEXES FORM.
HIGH TEMPERATURES CAUSE DENATURATION, DUE TO THE BREAKING OF BONDS HOLDING THE TERTIARY STRUCTURE TOGETHER, H-BONDS, DISULPHIDE BRIDGES, IONIC BONDS,
ACTIVE SITE ALTERED, CHANGES SHAPE, SUBSTRATE CANNOT BIND, NO ENZYME SUBSTRATE COMPLEXES FOREM.
CARBON DIOXIDE, CO2.
INCREASED LEVELS OF CARBON DIOXIDE, CO2, IN THE ATMOSPHERE ARE BELIEVED TO CONTRIBUTE TOWARDS CLIMATE CHNAGE, AS CARBON DIOXIDE, CO2, IS A GREENHOUSE GAS, AND IS INVOLVED IN THE GREENHOUSE EFFECT.
TEMPERATURE RECORDS.
ENABLE ANALYSIS, OF CHANGES IN TEMPERATURE.
EXTRAPOLATED DATA.
THE DATA CAN BE EXTRAPOLATED, TO MAKE PREDICTIONS WHICH CAN THEN BE USED IN MODELS OF FUTURE CLIMATE CHANGE.
SCUH MODELS HAVE LIMITATIONS, AS THEY DO NOT INCLUDE FACTORS INCLUDING HUMAN EFFORTS FOR THE REDUCTINO IN EMISSON OF GREENHOUSE GASES.
THE GREENHOUSE EFFECT.
THE GREENHOUSE EFFECT IS THE PROCESS IN WHICH:
SHORT-WAVELENGTH UV RADIATION PASSES THROUGH EARTH’S ATMOSPHERE AND IS REFLECTED FROM EARTH’S SURFACE.
THE REFLECTED RAYS ARE OF A LONGER WAVELENGTH, INFARED RADIATION, AND ARE TRAPPED BY GASES SUCH AS CARBON DIOXIDE, CO2, AND METHANE, CH4, THUS LEADING TO AN INCREASE IN THE TEMPERATURE OF THE EARTH’S SURFACE AND ATMOSPHERE.
CLIMATE CHANGE EFFECT, CHANGES IN DISTRIBUTION OF SPECIES.
CHANGES IN DISTRIBUSTION OF SPECIES, SPECIES WOULD MOVE TO COOILER AREAS, FOR EXAMPLE NORTHWARDS.
THIS COULD POTENTIALLT LEAD TO EXTINCTION OF SOME SPECIES DUE TO COMPETITION.