Planet Green

Ozone Depletion

noreply@blogger.com (sayantan.ritabrata) — Tue, 21 Oct 2008 10:30:00 +0000

Man-made chemicals have damaged the ozone layer that protects the earth from ultra violet (UV) radiation. We have phased out many ozone destroying chemicals but we’re still unsure how and when the ozone layer will recover.

What is ozone?
Ozone is a gas made of oxygen atoms. It can be found at ground level where it is a pollutant and a health hazard. But the useful ozone in the upper atmosphere, known as the ozone layer, is being destroyed. Here, ozone absorbs some of the potentially harmful ultraviolet radiation from the sun.

Which chemicals damage the ozone layer?
A group of chemicals known as halocarbons destroy ozone. The most familiar of these are chlorofluorocarbons (CFCs).
Aerosols and old refrigerators have released CFCs into the atmosphere. UV radiation breaks down CFCs in the upper stratosphere, releasing chlorine. Once released, chlorine becomes a catalyst of ozone destruction. A catalyst is something that makes a chemical reaction happen more easily, but it remains unchanged or reforms by the end of the reaction. It can then take part in the reaction again.
During this process, the ozone molecule is destroyed while the chlorine catalyst reforms. A single chlorine atom in the stratosphere can destroy about 100,000 ozone molecules.
The chemicals released into the upper atmosphere destroy ozone. However, pollution at ground level creates ozone, which can also affect life

How much of the ozone layer has been damaged?
In the past 30 years the ozone holes over the north and south poles have grown and shrunk.It was first suggested in 1974 that CFCs might damage the ozone layer. Scientists discovered a hole in the ozone layer over Antarctica in 1985. In September 2000, the ozone hole reached a record size of 30 million km2 - larger than North America. In September 2002, the ozone hole was just 15 million km2 - the smallest it has been since 1988.

Does the ozone layer damage affect the UK?
Yes. Ozone layer damage extends from the Arctic to northern Europe, including the UK. At Camborne in Cornwall and Lerwick in the Shetland Islands, total ozone concentrations have generally fallen since 1979 (suggesting ozone loss), although there has been an increase in recent years (Figure 1).
What are the effects of ozone loss?Declining ozone values mean UV levels have increased over the UK. UV exposure stops our immune systems working properly. We can develop eye cataracts and skin cancers. Deaths in England and Wales from malignant skin melanomas rose from 200 to 300 per year in the early 1950s to to 2167 in 2008.
UV radiation may also damage plants, and the young stages of aquatic wildlife.
What is being done to stop ozone layer damage? Industrialised countries have agreed to phase out halocarbons. Some critical uses are exempt and developing countries have been given longer time-scales. The UK did not stop CFC production until 2000.
By the late 1990s, atmospheric concentrations of other halocarbons had levelled out. Bromine concentrations should peak between 2000 and 2010, but will decline only slowly because a high proportion comes from uncontrolled sources, including the oceans.
HCFC (hydrochlorofluorocarbons) concentrations have increased from the early 1990s because they are used as a substitute for CFCs. Globally, HCFCs must be cut by 99.5% by 2020. They should begin to decline after 2010 as they are phased out. HCFCs will be banned in the European Union from 2015.
Stockpiled, recycled and illegally traded CFCs, together with those in refrigeration and fire-fighting equipment, will still be around for many years. The EU has regulations to prevent leaks of ozone depleting substances and promote recovery after use in industrial processes, although not in manufactured products.

Will ozone levels ever return to normal?
We don’t expect to see the signs of recovery in the ozone layer for 15 to 20 years. If the provisions of the Montreal Protocol on Substances that Deplete the Ozone Layer of 1987 are strengthened and followed, there is a prospect that the Antarctic ozone hole will be repaired by 2100. But greenhouse gases and changing global temperatures which are also altering the atmosphere make the nature of recovery uncertain. However, if the provisions of the Montreal Protocol are strengthened and followed, we could see the Antarctic ozone hole repaired by 2100.

noreply@blogger.com (sayantan.ritabrata) — Sun, 19 Oct 2008 07:18:00 +0000

Destabilization of local climates

In the northern hemisphere, the southern part of the Arctic region (home to 4,000,000 people) has experienced a temperature rise of 1 °C to 3 °C (1.8 °F to 5.4 °F) over the last 50 years. Canada, Alaska and Russia are experiencing initial melting of permafrost. This may disrupt ecosystems and by increasing bacterial activity in the soil lead to these areas becoming carbon sources instead of carbon sinks . A study (published in Science) of changes to eastern Siberia's permafrost suggests that it is gradually disappearing in the southern regions, leading to the loss of nearly 11% of Siberia's nearly 11,000 lakes since 1971 . At the same time, western Siberia is at the initial stage where melting permafrost is creating new lakes, which will eventually start disappearing as in the east. Furthermore, permafrost melting will eventually cause methane release from melting permafrost peat bogs.
Hurricanes were thought to be an entirely North Atlantic phenomenon. In late March 2004, the first Atlantic cyclone to form south of the equator hit Brazil with 40 m/s (144 km/h) winds, although some Brazilian meteorologists deny that it was a hurricane.Monitoring systems may have to be extended 1,600 km (1,000 miles) further south. There is no agreement as to whether this hurricane is linked to climate change, but one climate model exhibits increased tropical cyclone genesis in the South Atlantic under global warming by the end of the 21st century.

Polar Bears....soon a thing of the past

noreply@blogger.com (sayantan.ritabrata) — Wed, 01 Oct 2008 16:18:00 +0000

Polar Bear Listed in Endangered Species Act, but U.S. Government Limits Its Protection

The polar bear was officially listed as threatened under the U.S. endangered species act (ESA) on May 14, 2008. This the first creature brought under the act's protection for habitat loss that is linked to global warming. The official reason given was loss of Arctic sea ice and predictions that the ice will continue to decrease. Although global warming has been identified by most atmospheric and polar scientists as the main reason for Arctic warming and melting of sea ice, the U.S. Interior Department did not use this as a reason and clearly signaled it would not apply the law to greenhouse gas emissions.

Dirk Kempthorne, Interior Secretary, specifically said the listing would not prevent any sea ice from melting and that he would "make certain the ESA isn't abused to make global warming policies." This despite clear language in the ESA to control any activity causing harm to a listed species and requiring government agencies specifically not to jeopardize species by their actions. The wording of the listing document appears to be an attempt of the government to list the bear due to clear evidence of shrinking habitat yet not take all the steps to limit the loss. It seems analogous to President Bush's notorious "signing statements" limiting his acceptance of a Congressional law.

This could set up another court challenge by NGOs like the Center for Biological Diversity which originally brought the proposal and took the Interior Dept to court twice to get action.

"Threatened" under the ESA means a plant or animal may soon become endangered (at immediate risk of going extinct) if actions are not taken to protect it and its habitat.

Global Warming......Save us oh Mighty Lord

noreply@blogger.com (sayantan.ritabrata) — Wed, 01 Oct 2008 07:34:00 +0000

Global warming is the increase in the average measured temperature of the Earth's near-surface air and oceans since the mid-20th century, and its projected continuation.
The average global air temperature near the Earth's surface increased 0.74 ± 0.18 °C (1.33 ± 0.32 °F) during the 100 years ending in 2005. The Intergovernmental Panel on Climate Change (IPCC) concludes "most of the observed increase in globally averaged temperatures since the mid-twentieth century is very likely due to the observed increase in anthropogenic (man-made) greenhouse gas concentrations"via an enhanced greenhouse effect. Natural phenomena such as solar variation combined with volcanoes probably had a small warming effect from pre-industrial times to 1950 and a small cooling effect from 1950 onward.
These basic conclusions have been endorsed by at least 30 scientific societies and academies of science,including all of the national academies of science of the major industrialized countries.While individual scientists have voiced disagreement with some findings of the IPCC, the overwhelming majority of scientists working on climate change agree with the IPCC's main conclusions.
Climate model projections summarized by the IPCC indicate that average global surface temperature will likely rise a further 1.1 to 6.4 °C (2.0 to 11.5 °F) during the twenty-first century.This range of values results from the use of differing scenarios of future greenhouse gas emissions as well as models with differing climate sensitivity. Although most studies focus on the period up to 2100, warming and sea level rise are expected to continue for more than a thousand years even if greenhouse gas levels are stabilized. The delay in reaching equilibrium is a result of the large heat capacity of the oceans.
Increasing global temperature is expected to cause sea levels to rise, an increase in the intensity of extreme weather events, and significant changes to the amount and pattern of precipitation, likely leading to an expanse of tropical areas and increased pace of desertification. Other expected effects of global warming include changes in agricultural yields, modifications of trade routes, glacier retreat, mass species extinctions and increases in the ranges of disease vectors.
Remaining scientific uncertainties include the amount of warming expected in the future, and how warming and related changes will vary from region to region around the globe. Most national governments have signed and ratified the Kyoto Protocol aimed at reducing greenhouse gas emissions, but there is ongoing political and public debate worldwide regarding what, if any, action should be taken to reduce or reverse future warming or to adapt to its expected consequences.

noreply@blogger.com (sayantan.ritabrata) — Fri, 26 Sep 2008 15:39:00 +0000

The ecosystem concept
Main article: Ecosystem

The Daintree Rainforest in Queensland, Australia is an example of a forest ecosystem.
A central principle of ecology is that each living organism has an ongoing and continual relationship with every other element that makes up its environment. The sum total of interacting living organisms (the biocoenosis) and their non-living environment (the biotope) in an area is termed an ecosystem. Studies of ecosystems usually focus on the movement of energy and matter through the system.
Almost all ecosystems run on energy captured from the sun by primary producers via photosynthesis. This energy then flows through the food chains to primary consumers (herbivores who eat and digest the plants), and on to secondary and tertiary consumers (either carnivores or omnivores). Energy is lost to living organisms when it is used by the organisms to do work, or is lost as waste heat.
Matter is incorporated into living organisms by the primary producers. Photosynthetic plants fix carbon from carbon dioxide and nitrogen from atmospheric nitrogen or nitrates present in the soil to produce amino acids. Much of the carbon and nitrogen contained in ecosystems is created by such plants, and is then consumed by secondary and tertiary consumers and incorporated into themselves. Nutrients are usually returned to the ecosystem via decomposition. The entire movement of chemicals in an ecosystem is termed a biogeochemical cycle, and includes the carbon and nitrogen cycle.
Ecosystems of any size can be studied; for example, a rock and the plant life growing on it might be considered an ecosystem. This rock might be within a plain, with many such rocks, small grass, and grazing animals -- also an ecosystem. This plain might be in the tundra, which is also an ecosystem (although once they are of this size, they are generally termed ecozones or biomes). In fact, the entire terrestrial surface of the earth, all the matter which composes it, the air that is directly above it, and all the living organisms living within it can be considered as one, large ecosystem.
Ecosystems can be roughly divided into terrestrial ecosystems (including forest ecosystems, steppes, savannas, and so on), freshwater ecosystems (lakes, ponds and rivers), and marine ecosystems, depending on the dominant biotope.

Environment

noreply@blogger.com (sayantan.ritabrata) — Fri, 26 Sep 2008 15:26:00 +0000

Terminology and concept

Devil's Punchbowl Waterfall, New Zealand.

The terminology and concept of what comprises the natural environment includes a few key components:

Complete ecological units that function as natural systems without massive human intervention, including all vegetation, animals, microorganisms, rocks, atmosphere and natural phenomena that occur within their boundaries.

Universal natural resources and physical phenomena that lack clear-cut boundaries, such as air, water, and climate, as well as energy, radiation, electric charge, and magnetism, not originating from human activity.

The natural environment is contrasted with the built environment, which comprises the areas and components that are strongly influenced by man. A geographical area is regarded as a natural environment (with an indefinite article), if the human impact on it is kept under a certain limited level (similar to section 1 above). This level depends on the specific context, and changes in different areas and contexts. The term wilderness, on the other hand, refers to Earth that has not been modified by human activity.

Composition

Earth science (also known as geoscience, the geosciences or the Earth Sciences), is an all-embracing term for the sciences related to the planet Earth ^[1]. There are four major disciplines in earth sciences, namely geography, geology, geophysics and geodesy. These major disciplines use physics, chemistry, biology, chronology and mathematics to build a qualitative and quantitative understanding of the principal areas or spheres of the Earth system. Earth science generally recognizes 4 spheres, the lithosphere, the hydrosphere, the atmosphere, and the biosphere^[2]; these correspond to rocks, water, air, and life. Some practitioners include, as part of the spheres of the Earth, the cryosphere (corresponding to ice) as a distinct portion of the hydrosphere, as well as the pedosphere (corresponding to soil) as an active and intermixed sphere.

[edit] Geological activity

A volcanic fissure and lava channel.

The Earth's crust, or Continental crust, is the outermost solid land surface of the planet, is chemically and mechanically different from underlying mantles, and has been generated largely by igneous processes in which magma (molten rock) cools and solidifies to form solid land. Plate tectonics, mountain ranges, volcanoes, and earthquakes are geological phenomena that can be explained in terms of energy transformations in the Earth's crust^[3], and might be thought of as the process by which the earth resurfaces itself. Beneath the earth's crust lies the mantle which is heated by the radioactive decay of heavy elements. The mantle is not quite solid and consists of magma which is in a state of semi-perpetual convection. This convection process causes the lithospheric plates to move, albeit slowly. The resulting process is known as plate tectonics.^[4]^[5]^[6]^[7] Volcanoes result primarily from the melting of subducted crust material. Crust material that is forced into the Asthenosphere melts, and some portion of the melted material becomes light enough to rise to the surface, giving birth to volcanoes.^[5]

Oceanic activity

Polar bears on the sea ice of the Arctic Ocean, near the North Pole.

The shore of the Pacific Ocean in San Francisco, California.

An ocean is a major body of saline water, and a principal component of the hydrosphere. Approximately 71% of the Earth's surface (an area of some 361 million square kilometers) is covered by ocean, a continuous body of water that is customarily divided into several principal oceans and smaller seas. More than half of this area is over 3,000 meters (9,800 ft) deep. Average oceanic salinity is around 35 parts per thousand (ppt) (3.5%), and nearly all seawater has a salinity in the range of 30 to 38 ppt. Though generally recognized as several 'separate' oceans, these waters comprise one global, interconnected body of salt water often referred to as the World Ocean or global ocean.^[8]^[9] This concept of a global ocean as a continuous body of water with relatively free interchange among its parts is of fundamental importance to oceanography.^[10]

The major oceanic divisions are defined in part by the continents, various archipelagos, and other criteria: these divisions are (in descending order of size) the Pacific Ocean, the Atlantic Ocean, the Indian Ocean, the Southern Ocean (which is sometimes subsumed as the southern portions of the Pacific, Atlantic, and Indian Oceans), and the Arctic Ocean (which is sometimes considered a sea of the Atlantic). The Pacific and Atlantic may be further subdivided by the equator into northerly and southerly portions. Smaller regions of the oceans are called seas, gulfs, bays and other names. There are also salt lakes, which are smaller bodies of landlocked saltwater that are not interconnected with the World Ocean. Two notable examples of salt lakes are the Aral Sea and the Great Salt Lake.

Atmosphere, climate and weather

Main articles: Earth's atmosphere, climate, and weather

Atmospheric gases scatter blue light more than other wavelengths, creating a blue halo when seen from space.

The atmosphere of the Earth serves as a key factor in sustaining the planetary ecosystem. The thin layer of gases that envelops the Earth is held in place by the planet's gravity. Dry air consists of 78% nitrogen, 21% oxygen, 1% argon and other inert gases, carbon dioxide, etc.; but air also contains a variable amount of water vapor. The atmospheric pressure declines steadily with altitude, and has a scale height of about 8 kilometres at the Earth's surface: the height at which the atmospheric pressure has declined by a factor of e (a mathematical constant equal to 2.71...).^[11]^[12] The ozone layer of the Earth's atmosphere plays an important role in depleting the amount of ultraviolet (UV) radiation that reaches the surface. As DNA is readily damaged by UV light, this serves to protect life at the surface. The atmosphere also retains heat during the night, thereby reducing the daily temperature extremes.

Global warming effects

The retreat of Aletsch Glacier in the Swiss Alps (situation in 1979, 1991 and 2002), due to global warming.

Another view of the Aletsch Glacier in the Swiss Alps, which due to global warming, has been decreasing.

The potential dangers of global warming are being increasing studied by a wide global consortium of scientists, whom are increasingly concerned about the potential long-term effects of global warming on our natural environment and on the planet. Of particular concern is how climate change and global warming caused by anthropogenic, or human-made releases of greenhouse gases, most notably carbon dioxide, can act interactively, and have adverse effects upon the planet, it's natural environment and humans' existence. Efforts have been increasingly focused on the mitigation of greenhouse gases that are causing climatic changes, on developing adaptative strategies to global warming, to assist humans, animal and plant species, ecosystems, regions and nations in adjusting to the effects of global warming. Some examples of recent collaboration to address climate change and global warming include:

The United Nations Framework Convention Treaty and convention on Climate Change, to stabilize greenhouse gas concentrations in the atmosphere at a level that would prevent dangerous anthropogenic interference with the climate system.^[13]

The Kyoto Protocol), which is the protocol to the international Framework Convention on Climate Change treaty, again with the objective of reducing greenhouse gases in an effort to prevent anthropogenic climate change.^[14]

A significantly profound challenge is to identify the natural environmental dynamics in contrast to environmental changes not within natural variances. A common solution is to adapt a static view neglecting natural variances to exist. Methodologically, this view could be defended when looking at processes which change slowly and short time series, while the problem arrives when fast processes turns essential in the object of the study.

Life

Female mallard and ducklings - reproduction is essential for continuing life

Main articles: Life and Biosphere

Although there is no universal agreement on the definition of life, scientists generally accept that the biological manifestation of life is characterized by organization, metabolism, growth, adaptation, response to stimuli and reproduction.^[15] Life may also be said to be simply the characteristic state of organisms.

Properties common to terrestrial organisms (plants, animals, fungi, protists, archaea and bacteria) are that they are cellular, carbon-and-water-based with complex organization, having a metabolism, a capacity to grow, respond to stimuli, and reproduce. An entity with these properties is generally considered life. However, not every definition of life considers all of these properties to be essential. Human-made analogs of life may also be considered to be life.

The biosphere is the part of Earth's outer shell — including air, land, surface rocks and water — within which life occurs, and which biotic processes in turn alter or transform. From the broadest geophysiological point of view, the biosphere is the global ecological system integrating all living beings and their relationships, including their interaction with the elements of the lithosphere (rocks), hydrosphere (water), and atmosphere (air). Currently the entire Earth contains over 75 billion tons (150 trillion pounds or about 6.8 x 10¹³ kilograms) of biomass (life), which lives within various environments within the biosphere.^[16]

Ecosystems

A coral reef near the Hawaiian islands is an example of a complex marine ecosystem.

An ecosystem is a natural unit consisting of all plants, animals and micro-organisms (biotic factors) in an area functioning together with all of the non-living physical (abiotic) factors of the environment.^[17]

Central to the ecosystem concept is the idea that living organisms are continually engaged in a highly interrelated set of relationships with every other element constituting the environment in which they exist. Eugene Odum, one of the founders of the science of ecology, stated: "Any unit that includes all of the organisms (ie: the "community") in a given area interacting with the physical environment so that a flow of energy leads to clearly defined trophic structure, biotic diversity, and material cycles (ie: exchange of materials between living and nonliving parts) within the system is an ecosystem."^[18] The human ecosystem concept is then grounded in the deconstruction of the human/nature dichotomy, and the emergent premise that all species are ecologically integrated with each other, as well as with the abiotic constituents of their biotope.

Ecosystems can be bounded and discussed with tremendous variety of scope, and describe any situation where there is relationship between organisms and their environment. If humans are part of the organisms, one can speak of a 'human ecosystem'. As virtually no surface of the earth today is free of human contact, all ecosystems can be more accurately considered as human ecosystems, or more neutrally as human-influenced ecoystems.

Biomes

Map of Terrestrial biomes classified by vegetation.

Biomes are terminologically similar to the concept of ecosystems, and are climatically and geographically defined areas of ecologically similar climatic conditions such as communities of plants, animals, and soil organisms, often referred to as ecosystems. Biomes are defined based on factors such as plant structures (such as trees, shrubs, and grasses), leaf types (such as broadleaf and needleleaf), plant spacing (forest, woodland, savanna), and climate. Unlike ecozones, biomes are not defined by genetic, taxonomic, or historical similarities. Biomes are often identified with particular patterns of ecological succession and climax vegetation.

Wilderness

Wilderness is generally defined as a natural environment on Earth that has not been directly modified by human activity. Ecologists consider wilderness areas to be an integral part of the planet's self-sustaining natural ecosystem (the biosphere).

The word, "wilderness", derives from the notion of wildness; in other words that which is not controllable by humans. The word's etymology is from the Old English wildeornes, which in turn derives from wildeor meaning wild beast (wild + deor = beast, deer).^[19] From this point of view, it is the wildness of a place that makes it a wilderness. The mere presence or activity of people does not disqualify an area from being "wilderness." Many ecosystems that are, or have been, inhabited or influenced by activities of people may still be considered "wild." This way of looking at wilderness includes areas within which natural processes operate without very noticeable human interference.

Challenges

Summer field in Belgium (Hamois). The blue flower is Centaurea cyanus and the red one a Papaver rhoeas.

Before flue gas desulfurization was installed, the air-polluting emissions from this power plant in New Mexico contained excessive amounts of sulfur dioxide

It is the common understanding of natural environment that underlies environmentalism — a broad political, social, and philosophical movement that advocates various actions and policies in the interest of protecting what nature remains in the natural environment, or restoring or expanding the role of nature in this environment. While true wilderness is increasingly rare, wild nature (e.g., unmanaged forests, uncultivated grasslands, wildlife, wildflowers) can be found in many locations previously inhabited by humans.

Goals commonly expressed by environmental scientists include:

Reduction and clean up of pollution, with future goals of zero pollution;
Cleanly converting nonrecyclable materials into energy through direct combustion or after conversion into secondary fuels;
Reducing societal consumption of non-renewable fuels;
Development of alternative, green, low-carbon or renewable energy sources;
Conservation and sustainable use of scarce resources such as water, land, and air;
Protection of representative or unique or pristine ecosystems;
Preservation of threatened and endangered species extinction;
The establishment of nature and biosphere reserves under various types of protection; and, most generally, the protection of biodiversity and ecosystems upon which all human and other life on earth depends.

Very large development projects - megaprojects - pose special challenges and risks to the natural environment. Major dams and power plants are cases in point. The challenge to the environment from such projects is growing because more and bigger megaprojects are being built, in developed and developing nations alike.^[20]

Nature and biodiversity

noreply@blogger.com (sayantan.ritabrata) — Fri, 26 Sep 2008 07:07:00 +0000

Nature & Biodiversity
Biodiversity - the immense variety of Life on Earth - is what makes our planet not only habitable but beautiful. We depend on the natural richness of our planet for the food, energy, wood, raw materials, clean air and clean water that make life possible and which drive our economy. But we also look to our natural environment for less tangible things such as aesthetic pleasure, artistic inspiration and recreation.
The EU is committed to the protection of biodiversity; indeed there is a political commitment to halt biodiversity loss within the EU by 2010.
European society, our immense cultural diversity and our economies are reflected in our landscapes, agriculture and natural spaces. We are stewards of a wonderful natural legacy that we can pass on hopefully in tact to future generations. Over the last 25 years together we have built up a vast network of over 26,000 protected areas covering all the Member States and a total area of around 850.000 km2, representing more than 20% of total EU territory. This vast array of sites, known as the Natura 2000 network - the largest coherent network of protected areas in the world, is a testament to the importance that EU citizens attach to biodiversity.
The legal basis for the Natura 2000 network comes from the Birds Directive which dates back to 1979 and the Habitats Directive from 1991. Together these Directives constitute the backbone of the EU's internal policy on biodiversity protection. But protected nature areas do not exist and certainly cannot thrive in isolation from the rest of the land. We need to ensure that our agriculture as well as our regional, energy and transport policies are sustainable and that Europe's natural capital-its biodiversity, is conserved and protected.