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Environmental conditions play a key role in defining the function and distribution of plants, in
combination with other factors. Changes in long term environmental conditions that can be
collectively coined climate change are known to have had enormous impacts on plant diversity
patterns in the future and are seen as having significant current impacts. It is predicted that
climate change will remain one of the major drivers of biodiversity patterns in the future.
The Earth has experienced a constantly changing climate in the time since plants first evolved. In
comparison to the present day, this history has seen Earth as cooler, warmer, drier and wetter,
and CO2 (carbon dioxide) concentrations have been both higher and lower. These changes have
been reflected by constantly shifting vegetation, for example forest communities dominating
most areas in interglacial periods, and herbaceous communities dominating during glacial
periods. It has been shown that past climatic change has been a major driver of the processes of
speciation and extinction. The best known example of this is the Carboniferous Rainforest
Collapse which occurred 350 million years ago. This event decimated amphibian populations
and spurred on the evolution of reptiles
Greenhouse effect - the mechanism
The sun radiates solar energy on earth. The larger part of this energy (45%) is radiated back into
space. Greenhouse gases in the atmosphere contribute to global warming by adsorption and
reflection of atmospheric and solar energy. This natural phenomenon is what we call the
greenhouse effect. It is agreed that the greenhouse effect is correlated with global temperature
change. The primary greenhouse gases in the Earth’s atmosphere are water vapor, carbon
dioxide, methane, nitrous oxide, and ozone
Mechanism of global warming:
i. The incoming radiation from the Sun is mostly in the form of visible light and nearby
wavelengths, largely in the range 0.2 – 4 1m, corresponding to the Sun’s radioactive temperature
of 6,000 K. Almost half the radiation is in the form of “visible” light, which our eyes are adapted
to use.
ii. About 50% of the Sun’s energy is absorbed at the earth’s surface and the rest is reflected or
absorbed by the atmosphere. The reflection of light back into space – largely by clouds – does
not much affect the basic mechanism; this light, effectively, is lost to the system.
iii (a) Earth absorbs most of the sunlight it receives; The absorbed energy warms the surface; (b)
Earth then emits the absorbed light’s energy as infrared light; (c) greenhouse gases absorb a lot
of the infrared light before it can leave our atmosphere; (d) being absorbed slows the rate at
which energy escapes to space; and (e) the slower passage of energy heats up the atmosphere,
water, and ground. By increasing the amount of greenhouse gases in the atmosphere, humans are
increasing the atmosphere’s absorption of infrared light, thereby warming Earth and disrupting
global climate patterns.
Effects of CO2
Increases in atmospheric CO2 concentration affect how plants photosynthesize, resulting in
increases in plant water use efficiency, enhanced photosynthetic capacity and increased growth.
Increased CO2 has been implicated in ‘vegetation thickening’ which affects plant community
structure and function. Increased CO2 can also lead to increased Carbon:Nitrogen ratios in the
leaves of plants or in other aspects of leaf chemistry, possibly changing herbivore nutrition.
Effects of temperature
Increases in temperature raise the rate of many physiological processes such as photosynthesis in
plants, to an upper limit. Extreme temperatures can be harmful when beyond the physiological
limits of a plant.
Effects of water
Water supply is critical for plant growth; it plays a key role in determining the distribution of
plants. Changes in precipitation are predicted to be less consistent than for temperature and more
variable between regions, with predictions for some areas to become much wetter, and some
much drier. This can cause a major change in some ecosystems which are dependent on water
supply.
Agriculture
While CO2 is essential for plant growth, all agriculture depends also on steady water supplies,
and climate change is likely to disrupt those supplies through floods and droughts. It has been
suggested that higher latitudes – Siberia, for example – may become productive due to global
warming, but the soil in Arctic and bordering territories is very poor, and the amount of sunlight
reaching the ground in summer will not change because it is governed by the tilt of the earth.
Agriculture can also be disrupted by wildfires and changes in seasonal periodicity, which is
already taking place, and changes to grasslands and water supplies could impact grazing and
welfare of domestic livestock. Increased warming may also have a greater effect on countries
whose climate is already near or at a temperature limit over which yields reduce or crops fail – in
the tropics or sub-Sahara, for example.
Health
Warmer winters would mean fewer deaths, particularly among vulnerable groups like the aged.
However, the same groups are also vulnerable to additional heat, and deaths attributable to heat
waves are expected to be approximately five times as great as winter deaths prevented. It is
widely believed that warmer climates will encourage migration of disease-bearing insects like
mosquitoes and malaria is already appearing in places it hasn’t been seen before.
Polar melting
While the opening of a year-round ice free Arctic passage between the Atlantic and Pacific
oceans would confer some commercial benefits, these are considerably outweighed by the
negatives. Detrimental effects include loss of polar bear habitat and increased mobile ice hazards
to shipping. The loss of ice albedo (the reflection of heat), causing the ocean to absorb more heat,
is also a positive feedback; the warming waters increase glacier and Greenland ice cap melt, as
well as raising the temperature of Arctic tundra, which then releases methane, a very potent
greenhouse gas (methane is also released from the sea-bed, where it is trapped in ice-crystals
called clathrates). Melting of the Antarctic ice shelves is predicted to add further to sea-level rise
with no benefits accruing.
Ocean acidification
A cause for considerable concern, there appears to be no benefits to the change in pH of the
oceans. This process is caused by additional CO2 being absorbed in the water, and may have
severe destabilising effects on the entire oceanic food-chain.
Melting glaciers
The effects of glaciers melting are largely detrimental; the principle impact being that many
millions of people (one-sixth of the world’s population) depend on fresh water supplied each
year by natural spring melt and regrowth cycles and those water supplies – drinking water,
agriculture – may fail.
Sea level rise
Many parts of the world are low-lying and will be severely affected by modest sea rises. Rice
paddies are being inundated with salt water, which destroys the crops. Seawater is contaminating
rivers as it mixes with fresh water further upstream, and aquifers are becoming polluted. Given
that the IPCC did not include melt-water from the Greenland and Antarctic ice-caps due to
uncertainties at that time, estimates of sea-level rise are feared to considerably underestimate the
scale of the problem. There are no proposed benefits to sea-level rise.
Positives and negatives of global warming
Positive effects of climate change may include greener rainforests and enhanced plant growth in
the Amazon, increased vegetation in northern latitudes and possible increases in plankton
biomass in some parts of the ocean.
Negative responses may include further growth of oxygen poor ocean zones, contamination or
exhaustion of fresh water, increased incidence of natural fires, extensive vegetation die-off due
to droughts, increased risk of coral extinction, decline in global phytoplankton, changes in
migration patterns of birds and animals, changes in seasonal periodicity, disruption to food
chains and species loss.
Solution
Environmental conditions play a key role in defining the function and distribution of plants, in
combination with other factors. Changes in long term environmental conditions that can be
collectively coined climate change are known to have had enormous impacts on plant diversity
patterns in the future and are seen as having significant current impacts. It is predicted that
climate change will remain one of the major drivers of biodiversity patterns in the future.
The Earth has experienced a constantly changing climate in the time since plants first evolved. In
comparison to the present day, this history has seen Earth as cooler, warmer, drier and wetter,
and CO2 (carbon dioxide) concentrations have been both higher and lower. These changes have
been reflected by constantly shifting vegetation, for example forest communities dominating
most areas in interglacial periods, and herbaceous communities dominating during glacial
periods. It has been shown that past climatic change has been a major driver of the processes of
speciation and extinction. The best known example of this is the Carboniferous Rainforest
Collapse which occurred 350 million years ago. This event decimated amphibian populations
and spurred on the evolution of reptiles
Greenhouse effect - the mechanism
The sun radiates solar energy on earth. The larger part of this energy (45%) is radiated back into
space. Greenhouse gases in the atmosphere contribute to global warming by adsorption and
reflection of atmospheric and solar energy. This natural phenomenon is what we call the
greenhouse effect. It is agreed that the greenhouse effect is correlated with global temperature
change. The primary greenhouse gases in the Earth’s atmosphere are water vapor, carbon
dioxide, methane, nitrous oxide, and ozone
Mechanism of global warming:
i. The incoming radiation from the Sun is mostly in the form of visible light and nearby
wavelengths, largely in the range 0.2 – 4 1m, corresponding to the Sun’s radioactive temperature
of 6,000 K. Almost half the radiation is in the form of “visible” light, which our eyes are adapted
to use.
ii. About 50% of the Sun’s energy is absorbed at the earth’s surface and the rest is reflected or
absorbed by the atmosphere. The reflection of light back into space – largely by clouds – does
not much affect the basic mechanism; this light, effectively, is lost to the system.
iii (a) Earth absorbs most of the sunlight it receives; The absorbed energy warms the surface; (b)
Earth then emits the absorbed light’s energy as infrared light; (c) greenhouse gases absorb a lot
of the infrared light before it can leave our atmosphere; (d) being absorbed slows the rate at
which energy escapes to space; and (e) the slower passage of energy heats up the atmosphere,
water, and ground. By increasing the amount of greenhouse gases in the atmosphere, humans are
increasing the atmosphere’s absorption of infrared light, thereby warming Earth and disrupting
global climate patterns.
Effects of CO2
Increases in atmospheric CO2 concentration affect how plants photosynthesize, resulting in
increases in plant water use efficiency, enhanced photosynthetic capacity and increased growth.
Increased CO2 has been implicated in ‘vegetation thickening’ which affects plant community
structure and function. Increased CO2 can also lead to increased Carbon:Nitrogen ratios in the
leaves of plants or in other aspects of leaf chemistry, possibly changing herbivore nutrition.
Effects of temperature
Increases in temperature raise the rate of many physiological processes such as photosynthesis in
plants, to an upper limit. Extreme temperatures can be harmful when beyond the physiological
limits of a plant.
Effects of water
Water supply is critical for plant growth; it plays a key role in determining the distribution of
plants. Changes in precipitation are predicted to be less consistent than for temperature and more
variable between regions, with predictions for some areas to become much wetter, and some
much drier. This can cause a major change in some ecosystems which are dependent on water
supply.
Agriculture
While CO2 is essential for plant growth, all agriculture depends also on steady water supplies,
and climate change is likely to disrupt those supplies through floods and droughts. It has been
suggested that higher latitudes – Siberia, for example – may become productive due to global
warming, but the soil in Arctic and bordering territories is very poor, and the amount of sunlight
reaching the ground in summer will not change because it is governed by the tilt of the earth.
Agriculture can also be disrupted by wildfires and changes in seasonal periodicity, which is
already taking place, and changes to grasslands and water supplies could impact grazing and
welfare of domestic livestock. Increased warming may also have a greater effect on countries
whose climate is already near or at a temperature limit over which yields reduce or crops fail – in
the tropics or sub-Sahara, for example.
Health
Warmer winters would mean fewer deaths, particularly among vulnerable groups like the aged.
However, the same groups are also vulnerable to additional heat, and deaths attributable to heat
waves are expected to be approximately five times as great as winter deaths prevented. It is
widely believed that warmer climates will encourage migration of disease-bearing insects like
mosquitoes and malaria is already appearing in places it hasn’t been seen before.
Polar melting
While the opening of a year-round ice free Arctic passage between the Atlantic and Pacific
oceans would confer some commercial benefits, these are considerably outweighed by the
negatives. Detrimental effects include loss of polar bear habitat and increased mobile ice hazards
to shipping. The loss of ice albedo (the reflection of heat), causing the ocean to absorb more heat,
is also a positive feedback; the warming waters increase glacier and Greenland ice cap melt, as
well as raising the temperature of Arctic tundra, which then releases methane, a very potent
greenhouse gas (methane is also released from the sea-bed, where it is trapped in ice-crystals
called clathrates). Melting of the Antarctic ice shelves is predicted to add further to sea-level rise
with no benefits accruing.
Ocean acidification
A cause for considerable concern, there appears to be no benefits to the change in pH of the
oceans. This process is caused by additional CO2 being absorbed in the water, and may have
severe destabilising effects on the entire oceanic food-chain.
Melting glaciers
The effects of glaciers melting are largely detrimental; the principle impact being that many
millions of people (one-sixth of the world’s population) depend on fresh water supplied each
year by natural spring melt and regrowth cycles and those water supplies – drinking water,
agriculture – may fail.
Sea level rise
Many parts of the world are low-lying and will be severely affected by modest sea rises. Rice
paddies are being inundated with salt water, which destroys the crops. Seawater is contaminating
rivers as it mixes with fresh water further upstream, and aquifers are becoming polluted. Given
that the IPCC did not include melt-water from the Greenland and Antarctic ice-caps due to
uncertainties at that time, estimates of sea-level rise are feared to considerably underestimate the
scale of the problem. There are no proposed benefits to sea-level rise.
Positives and negatives of global warming
Positive effects of climate change may include greener rainforests and enhanced plant growth in
the Amazon, increased vegetation in northern latitudes and possible increases in plankton
biomass in some parts of the ocean.
Negative responses may include further growth of oxygen poor ocean zones, contamination or
exhaustion of fresh water, increased incidence of natural fires, extensive vegetation die-off due
to droughts, increased risk of coral extinction, decline in global phytoplankton, changes in
migration patterns of birds and animals, changes in seasonal periodicity, disruption to food
chains and species loss.

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Environmental conditions play a key role in defining the function an.pdf

  • 1. Environmental conditions play a key role in defining the function and distribution of plants, in combination with other factors. Changes in long term environmental conditions that can be collectively coined climate change are known to have had enormous impacts on plant diversity patterns in the future and are seen as having significant current impacts. It is predicted that climate change will remain one of the major drivers of biodiversity patterns in the future. The Earth has experienced a constantly changing climate in the time since plants first evolved. In comparison to the present day, this history has seen Earth as cooler, warmer, drier and wetter, and CO2 (carbon dioxide) concentrations have been both higher and lower. These changes have been reflected by constantly shifting vegetation, for example forest communities dominating most areas in interglacial periods, and herbaceous communities dominating during glacial periods. It has been shown that past climatic change has been a major driver of the processes of speciation and extinction. The best known example of this is the Carboniferous Rainforest Collapse which occurred 350 million years ago. This event decimated amphibian populations and spurred on the evolution of reptiles Greenhouse effect - the mechanism The sun radiates solar energy on earth. The larger part of this energy (45%) is radiated back into space. Greenhouse gases in the atmosphere contribute to global warming by adsorption and reflection of atmospheric and solar energy. This natural phenomenon is what we call the greenhouse effect. It is agreed that the greenhouse effect is correlated with global temperature change. The primary greenhouse gases in the Earth’s atmosphere are water vapor, carbon dioxide, methane, nitrous oxide, and ozone Mechanism of global warming: i. The incoming radiation from the Sun is mostly in the form of visible light and nearby wavelengths, largely in the range 0.2 – 4 1m, corresponding to the Sun’s radioactive temperature of 6,000 K. Almost half the radiation is in the form of “visible” light, which our eyes are adapted to use. ii. About 50% of the Sun’s energy is absorbed at the earth’s surface and the rest is reflected or absorbed by the atmosphere. The reflection of light back into space – largely by clouds – does not much affect the basic mechanism; this light, effectively, is lost to the system. iii (a) Earth absorbs most of the sunlight it receives; The absorbed energy warms the surface; (b) Earth then emits the absorbed light’s energy as infrared light; (c) greenhouse gases absorb a lot of the infrared light before it can leave our atmosphere; (d) being absorbed slows the rate at which energy escapes to space; and (e) the slower passage of energy heats up the atmosphere, water, and ground. By increasing the amount of greenhouse gases in the atmosphere, humans are increasing the atmosphere’s absorption of infrared light, thereby warming Earth and disrupting
  • 2. global climate patterns. Effects of CO2 Increases in atmospheric CO2 concentration affect how plants photosynthesize, resulting in increases in plant water use efficiency, enhanced photosynthetic capacity and increased growth. Increased CO2 has been implicated in ‘vegetation thickening’ which affects plant community structure and function. Increased CO2 can also lead to increased Carbon:Nitrogen ratios in the leaves of plants or in other aspects of leaf chemistry, possibly changing herbivore nutrition. Effects of temperature Increases in temperature raise the rate of many physiological processes such as photosynthesis in plants, to an upper limit. Extreme temperatures can be harmful when beyond the physiological limits of a plant. Effects of water Water supply is critical for plant growth; it plays a key role in determining the distribution of plants. Changes in precipitation are predicted to be less consistent than for temperature and more variable between regions, with predictions for some areas to become much wetter, and some much drier. This can cause a major change in some ecosystems which are dependent on water supply. Agriculture While CO2 is essential for plant growth, all agriculture depends also on steady water supplies, and climate change is likely to disrupt those supplies through floods and droughts. It has been suggested that higher latitudes – Siberia, for example – may become productive due to global warming, but the soil in Arctic and bordering territories is very poor, and the amount of sunlight reaching the ground in summer will not change because it is governed by the tilt of the earth. Agriculture can also be disrupted by wildfires and changes in seasonal periodicity, which is already taking place, and changes to grasslands and water supplies could impact grazing and welfare of domestic livestock. Increased warming may also have a greater effect on countries whose climate is already near or at a temperature limit over which yields reduce or crops fail – in the tropics or sub-Sahara, for example. Health Warmer winters would mean fewer deaths, particularly among vulnerable groups like the aged. However, the same groups are also vulnerable to additional heat, and deaths attributable to heat waves are expected to be approximately five times as great as winter deaths prevented. It is widely believed that warmer climates will encourage migration of disease-bearing insects like mosquitoes and malaria is already appearing in places it hasn’t been seen before. Polar melting While the opening of a year-round ice free Arctic passage between the Atlantic and Pacific
  • 3. oceans would confer some commercial benefits, these are considerably outweighed by the negatives. Detrimental effects include loss of polar bear habitat and increased mobile ice hazards to shipping. The loss of ice albedo (the reflection of heat), causing the ocean to absorb more heat, is also a positive feedback; the warming waters increase glacier and Greenland ice cap melt, as well as raising the temperature of Arctic tundra, which then releases methane, a very potent greenhouse gas (methane is also released from the sea-bed, where it is trapped in ice-crystals called clathrates). Melting of the Antarctic ice shelves is predicted to add further to sea-level rise with no benefits accruing. Ocean acidification A cause for considerable concern, there appears to be no benefits to the change in pH of the oceans. This process is caused by additional CO2 being absorbed in the water, and may have severe destabilising effects on the entire oceanic food-chain. Melting glaciers The effects of glaciers melting are largely detrimental; the principle impact being that many millions of people (one-sixth of the world’s population) depend on fresh water supplied each year by natural spring melt and regrowth cycles and those water supplies – drinking water, agriculture – may fail. Sea level rise Many parts of the world are low-lying and will be severely affected by modest sea rises. Rice paddies are being inundated with salt water, which destroys the crops. Seawater is contaminating rivers as it mixes with fresh water further upstream, and aquifers are becoming polluted. Given that the IPCC did not include melt-water from the Greenland and Antarctic ice-caps due to uncertainties at that time, estimates of sea-level rise are feared to considerably underestimate the scale of the problem. There are no proposed benefits to sea-level rise. Positives and negatives of global warming Positive effects of climate change may include greener rainforests and enhanced plant growth in the Amazon, increased vegetation in northern latitudes and possible increases in plankton biomass in some parts of the ocean. Negative responses may include further growth of oxygen poor ocean zones, contamination or exhaustion of fresh water, increased incidence of natural fires, extensive vegetation die-off due to droughts, increased risk of coral extinction, decline in global phytoplankton, changes in migration patterns of birds and animals, changes in seasonal periodicity, disruption to food chains and species loss. Solution
  • 4. Environmental conditions play a key role in defining the function and distribution of plants, in combination with other factors. Changes in long term environmental conditions that can be collectively coined climate change are known to have had enormous impacts on plant diversity patterns in the future and are seen as having significant current impacts. It is predicted that climate change will remain one of the major drivers of biodiversity patterns in the future. The Earth has experienced a constantly changing climate in the time since plants first evolved. In comparison to the present day, this history has seen Earth as cooler, warmer, drier and wetter, and CO2 (carbon dioxide) concentrations have been both higher and lower. These changes have been reflected by constantly shifting vegetation, for example forest communities dominating most areas in interglacial periods, and herbaceous communities dominating during glacial periods. It has been shown that past climatic change has been a major driver of the processes of speciation and extinction. The best known example of this is the Carboniferous Rainforest Collapse which occurred 350 million years ago. This event decimated amphibian populations and spurred on the evolution of reptiles Greenhouse effect - the mechanism The sun radiates solar energy on earth. The larger part of this energy (45%) is radiated back into space. Greenhouse gases in the atmosphere contribute to global warming by adsorption and reflection of atmospheric and solar energy. This natural phenomenon is what we call the greenhouse effect. It is agreed that the greenhouse effect is correlated with global temperature change. The primary greenhouse gases in the Earth’s atmosphere are water vapor, carbon dioxide, methane, nitrous oxide, and ozone Mechanism of global warming: i. The incoming radiation from the Sun is mostly in the form of visible light and nearby wavelengths, largely in the range 0.2 – 4 1m, corresponding to the Sun’s radioactive temperature of 6,000 K. Almost half the radiation is in the form of “visible” light, which our eyes are adapted to use. ii. About 50% of the Sun’s energy is absorbed at the earth’s surface and the rest is reflected or absorbed by the atmosphere. The reflection of light back into space – largely by clouds – does not much affect the basic mechanism; this light, effectively, is lost to the system. iii (a) Earth absorbs most of the sunlight it receives; The absorbed energy warms the surface; (b) Earth then emits the absorbed light’s energy as infrared light; (c) greenhouse gases absorb a lot of the infrared light before it can leave our atmosphere; (d) being absorbed slows the rate at which energy escapes to space; and (e) the slower passage of energy heats up the atmosphere, water, and ground. By increasing the amount of greenhouse gases in the atmosphere, humans are increasing the atmosphere’s absorption of infrared light, thereby warming Earth and disrupting global climate patterns.
  • 5. Effects of CO2 Increases in atmospheric CO2 concentration affect how plants photosynthesize, resulting in increases in plant water use efficiency, enhanced photosynthetic capacity and increased growth. Increased CO2 has been implicated in ‘vegetation thickening’ which affects plant community structure and function. Increased CO2 can also lead to increased Carbon:Nitrogen ratios in the leaves of plants or in other aspects of leaf chemistry, possibly changing herbivore nutrition. Effects of temperature Increases in temperature raise the rate of many physiological processes such as photosynthesis in plants, to an upper limit. Extreme temperatures can be harmful when beyond the physiological limits of a plant. Effects of water Water supply is critical for plant growth; it plays a key role in determining the distribution of plants. Changes in precipitation are predicted to be less consistent than for temperature and more variable between regions, with predictions for some areas to become much wetter, and some much drier. This can cause a major change in some ecosystems which are dependent on water supply. Agriculture While CO2 is essential for plant growth, all agriculture depends also on steady water supplies, and climate change is likely to disrupt those supplies through floods and droughts. It has been suggested that higher latitudes – Siberia, for example – may become productive due to global warming, but the soil in Arctic and bordering territories is very poor, and the amount of sunlight reaching the ground in summer will not change because it is governed by the tilt of the earth. Agriculture can also be disrupted by wildfires and changes in seasonal periodicity, which is already taking place, and changes to grasslands and water supplies could impact grazing and welfare of domestic livestock. Increased warming may also have a greater effect on countries whose climate is already near or at a temperature limit over which yields reduce or crops fail – in the tropics or sub-Sahara, for example. Health Warmer winters would mean fewer deaths, particularly among vulnerable groups like the aged. However, the same groups are also vulnerable to additional heat, and deaths attributable to heat waves are expected to be approximately five times as great as winter deaths prevented. It is widely believed that warmer climates will encourage migration of disease-bearing insects like mosquitoes and malaria is already appearing in places it hasn’t been seen before. Polar melting While the opening of a year-round ice free Arctic passage between the Atlantic and Pacific oceans would confer some commercial benefits, these are considerably outweighed by the
  • 6. negatives. Detrimental effects include loss of polar bear habitat and increased mobile ice hazards to shipping. The loss of ice albedo (the reflection of heat), causing the ocean to absorb more heat, is also a positive feedback; the warming waters increase glacier and Greenland ice cap melt, as well as raising the temperature of Arctic tundra, which then releases methane, a very potent greenhouse gas (methane is also released from the sea-bed, where it is trapped in ice-crystals called clathrates). Melting of the Antarctic ice shelves is predicted to add further to sea-level rise with no benefits accruing. Ocean acidification A cause for considerable concern, there appears to be no benefits to the change in pH of the oceans. This process is caused by additional CO2 being absorbed in the water, and may have severe destabilising effects on the entire oceanic food-chain. Melting glaciers The effects of glaciers melting are largely detrimental; the principle impact being that many millions of people (one-sixth of the world’s population) depend on fresh water supplied each year by natural spring melt and regrowth cycles and those water supplies – drinking water, agriculture – may fail. Sea level rise Many parts of the world are low-lying and will be severely affected by modest sea rises. Rice paddies are being inundated with salt water, which destroys the crops. Seawater is contaminating rivers as it mixes with fresh water further upstream, and aquifers are becoming polluted. Given that the IPCC did not include melt-water from the Greenland and Antarctic ice-caps due to uncertainties at that time, estimates of sea-level rise are feared to considerably underestimate the scale of the problem. There are no proposed benefits to sea-level rise. Positives and negatives of global warming Positive effects of climate change may include greener rainforests and enhanced plant growth in the Amazon, increased vegetation in northern latitudes and possible increases in plankton biomass in some parts of the ocean. Negative responses may include further growth of oxygen poor ocean zones, contamination or exhaustion of fresh water, increased incidence of natural fires, extensive vegetation die-off due to droughts, increased risk of coral extinction, decline in global phytoplankton, changes in migration patterns of birds and animals, changes in seasonal periodicity, disruption to food chains and species loss.