What Weather Means?
Weather is basically the way the atmosphere is behaving, mainly with respect to its effects upon life and human activities. Weather consists of the short-term, minutes to months, changes in the atmosphere. Most people think of weather in terms of temperature, humidity, precipitation, cloudiness, brightness, visibility, wind, and atmospheric pressure, as in high and low pressure. In most places, weather can change from minute-to-minute, hour-to-hour, day-to-day, and season-to-season.
Scientifically, Weather is the state of atmosphere at a particular time and place.
Elements of Weather
Weather is described in terms of variable conditions such as temperature, humidity, wind velocity, precipitation, and barometric pressure. Weather on Earth occurs primarily in the troposphere, or lower atmosphere, and is driven by energy from the Sun and the rotation of the Earth. The average weather conditions of a region over time are used to define a region's climate.
National weather services
In order to help people be prepared to face all of these, the National Oceanic and Atmospheric Administration's (NOAA) National Weather Service (NWS), the lead forecasting outlet for the nation's weather, has over 25 different types of warnings, statements or watches that they issue. Some of the reports NWS issues are: Flash Flood Watches and Warnings, Severe Thunderstorm Watches and Warnings, Blizzard Warnings, Snow Advisories, Winter Storm Watches and Warnings, Dense Fog Advisory, Fire Weather Watch, Tornado Watches and Warnings, Hurricane Watches and Warnings. They also provide Special Weather Statements and Short and Long Term Forecasts.
NWS also issues a lot of notices concerning marine weather for boaters and others who dwell or are staying near shorelines. They include: Coastal Flood Watches and Warnings, Flood Watches and Warnings, High Wind Warnings, Wind Advisories, Gale Warnings, High Surf Advisories, Heavy Freezing Spray Warnings, Small Craft Advisories, Marine Weather Statements, Freezing Fog Advisories, Coastal Flood Watches, Flood Statements, Coastal Flood Statement.
According to their mission statement, "The National Weather Service provides weather, hydrologic, and climate forecasts and warnings for the United States, its territories, adjacent waters and ocean areas, for the protection of life and property and the enhancement of the national economy. NWS data and products form a national information database and infrastructure which can be used by other governmental agencies, the private sector, the public, and the global community."
What causes weather?

Because the Earth is round and not flat, the Sun's rays don't fall evenly on the land and oceans. The Sun shines more directly near the equator bringing these areas more warmth. However, the Polar Regions are at such an angle to the Sun that they get little or no sunlight during the winter, causing colder temperatures. These differences in temperature create a restless movement of air and water in great swirling currents to distribute heat energy from the Sun across the planet. When air in one region is warmer than the surrounding air, it becomes less dense and begins to rise, drawing more air in underneath. Elsewhere, cooler denser air sinks, pushing air outward to flow along the surface and complete the cycle.

Climate
As many of us already know, Climate is the average weather usually taken over a 30-year time period for a particular region and time period. It is a point that climate is not the same as weather, but rather, it is the average pattern of weather for a particular region.
Or in short, we can say, that climate is the description of the long-term pattern of weather in a particular area. It is really an average pattern of weather for a particular region.
When scientists talk about climate, they're looking at averages of precipitation, temperature, humidity, sunshine, wind velocity, phenomena such as fog, frost, and hail storms, and other measures of the weather that occur over a long period in a particular place.
For example, after looking at rain gauge data, lake and reservoir levels, and satellite data, scientists can tell if during a summer, an area was drier than average.

What is our climate system?
As we all know the atmosphere covers the Earth. It is a thin layer of mixed gases which make up the air we breathe. This thin layer also helps the Earth from becoming too hot or too cold.
Ocean cover is about 70 percent of Earth's surface. Their large size and thermal properties allow them to store a lot of heat.
Land covers 27 percent of Earth's surface and land topography influences weather patterns.
Ice is the world's largest supply of freshwater. It covers the remaining 3 percent of Earth's surface including most of Antarctica and Greenland. Ice plays an important role in regulating climate, because it is highly reflective.


Climate, Science, and Record Keeping
Global change research is one of the most important contemporary applications of climate data. Historical records are used to document trends and test climate prediction models. One of the most challenging aspects of climate change detection is distinguishing natural long-term variations from trends caused by human activity. Many other research disciplines also depend upon climate records. These include most major branches of the life sciences, and many applied aspects and some pure research topics in the physical and geophysical sciences, such as geology.
Climate is an integral part of the geological and biological history of planet Earth. In this sense, the value of climate records transcends pure economics and adds an aesthetic dimension that cannot be easily quantified. The spirit of this assertion is implicit in the name that the early climatologists gave to periodic summaries of weather statistics: The Decennial Census of the Climate.
The National Climatic Data Centre (NCDC) is the place of collection of global weather records. In addition to the varied information and data services provided by the NCDC, research is conducted to go through challenges ranging from assessing global warming to helping local ferry services.
Let us now know about three main climatic regions of the world.
Tundra Region
The tundra region is located in the Arctic, around the North Pole and covers 1/5 of Earth's surface. They have very harsh, cold, long winters and very short, cool summers. The winter temperatures can fall as low as -60°F.  The summer month temperatures range between 32°F to 50°F. The most distinctive feature about the tundra region is the frozen soil called permafrost. This region is treeless with very little vegetation. Very little precipitation occurs in the tundra region, usually less than 10" per year.
The tundra lies near the North Pole. However, there are also areas called alpine tundra, located at the top of cold mountains.
Tropical Region
The west coastal lowlands, the Western Ghats, and southern parts of Assam have this climate type. It is characterized by high temperatures throughout the year, even in the hills. The rainfall here is seasonal, but heavy and is above 78 cm in a year. Most of the rain is received in the period from May to November, and is adequate for the growth of vegetation during the entire year. December to March are the dry months with very little rainfall. The heavy rain is responsible for the tropical wet forests in these regions, which consists of a large number of species of animals. Evergreen forests are the typical feature of the region.
Sub Tropical Region
The subtropics are geographic and climate zones located roughly between the tropic circle of latitude (the Tropic of Cancer and Tropic of Capricorn) and the 35th parallel in each hemisphere. Subtropical climate regimes can exist at high elevations within the tropics, such as across the Mexican Plateau and in Vietnam and Taiwan. Six climate classifications utilize the term to help define the various temperature and precipitation regimes for the planet Earth.
 Who Uses Climate Information?
Almost every economic activity is sensitive to climate. Let us know about some.
Business is a large consumer of climatic information. Effective marketing strategies target advertising when potential demand is greatest. That means selling rain gear when it's rainy, snow gear when it's snowy and recreation products when it's sunny.
In agriculture and horticulture, the needs for climate information are obvious. The duration of the growing season depends on plant type and air temperature. Both livestock and crops depend on the availability of water, which is usually derived from local or watershed precipitation.
Architects and structural engineers need to know factors such as wind loading; snow loads for roofing; precipitation for drainage and lawn watering systems; temperature statistics for heating, air conditioning, and frost penetration for foundations and water pipes; icing for wires and other exposed structures; and flood frequency to ensure safe construction at elevations above oceans, lakes, or streams. These factors are particularly important when large, expensive structures are built and when large communities of new homes are constructed.
The transportation industry is also one of the large consumers of climatic data. You may wonder how? So let me tell you, Commercial aviation has been one of the primary forces for standardized and improved national weather and climate services worldwide. Indeed, strong aviation interest in weather. At that time, flight schedules and safety considerations were even more critical for aviation than they are today. Climate data are used extensively in airport design and aeronautical engineering. Wind direction and speed, visibility, air pressure, temperature, icing frequency, cloud cover, humidity, the character of the air (fog, haze, smoke, and dust storms for example), and other elements are significant. There are also many uses for climate information in the shipping industry and in recreational boating.
In such way, in every field climatic information is required at a good scale in order to head towards success.

What causes changes in weather?

All changes in the weather are caused by the sun. The sun is a huge sphere of hot gases at a very high temperature. The distance of the sun from us is very large. Even then the energy sent out by the sun is so huge that it is the source of all heat and light on the earth. So, the sun is the primary source of energy that causes changes in the weather. Energy absorbed and reflected by the earth’s surface, oceans and the atmosphere play important roles in determining the weather at any place. If you live near the sea, you would have realised that the weather at your place is different from that of a place in a desert, or near a mountain.

Adaptation in Polar Regions

The Polar Regions present an extreme climate. These regions are covered with snow and it is very cold for most part of the year. For six months the sun does not set at the poles while for the other six months the sun does not rise. In winters, the temperature can be as low as –37°C. Animals living there have adapted to these severe conditions. Let us see how they are adapted by considering the examples of polar bears and penguins. Polar bears have white fur so that they are not easily visible in the snowy white background. It protects them from their predators. It also helps them in catching their prey. To protect them from extreme cold, they have two thick layers of fur. They also have a layer of fat under their skin. In fact, they are so well-insulated that they have to move slowly and rest often to avoid getting overheated.

Physical activities on warm days necessitate cooling. So, the polar bear goes for swimming. It is a good swimmer. Its paws are wide and large, which help it not only to swim well but also walk with ease in the snow. While swimming under water, it can close its nostrils and can remain under water for long durations. It has a strong sense of smell so that it can catch its prey for food.

Migration

Migration is the movement of living organisms from one place to another.

Migration can be permanent, temporary, voluntary or forced. It can be international or internal.

Also we may say that migration is to pass usually periodically from one region or climate to another for feeding or breeding. It is one of the means to escape the harsh, cold conditions.

Migratory Birds

Some migratory birds travel as much as 15000 km to escape the extreme climatic conditions at home. Generally they fly high where the wind flow is helpful and the cold conditions allow them to disperse the heat generated by their flight muscles. But how these birds travel to the same place year after year is still a mystery. It seems that these birds have a built–in sense of direction and know in which direction to travel. Some birds probably use landmarks to guide them. Many birds may be guided by the sun during the day and stars at night. There is some evidence that birds may use the magnetic field of the earth to find direction. And it is not only birds that migrate; mammals, many types of fish and insects are also known to migrate seasonally in search of more hospitable climates.

Why is there a large population in tropical rainforests?

The tropical region has generally a hot climate because of its location around the equator. Even in the coldest month the temperature is generally higher than about 15°C. During hot summers, the temperature may cross 40°C. Days and nights are almost equal in length throughout the year. These regions get plenty of rainfall. An important feature of this region is the tropical rainforests. Tropical rainforests are found in Western Ghats and Assam in India, Southeast Asia, Central America and Central Africa. Because of continuous warmth and rain, this region supports wide variety of plants and animals. The major types of animals living in the rainforests are monkeys, apes, gorillas, tigers, elephants, leopards, lizards, snakes, birds and insects. The climatic conditions in rainforests are highly suitable for supporting an enormous number and a variety of animals.

Adaptations of Animals in Tropical Rainforests

Red-eyed frog has developed sticky pads on its feet to help it climb trees on which it lives. To help them live on the trees, monkeys have long tails for grasping branches. Their hands and feet are such that they can easily hold on to the branches.

As there is competition for food, some animals are adapted to get food not easily reachable. A striking example is that of the bird Toucan, which possesses a long, large beak. This helps a toucan to reach the fruits on branches which are otherwise too weak to support its weight.

Many tropical animals have sensitive hearing, sharp eyesight, thick skin and a skin colour which helps them to camouflage by blending with the surroundings. This is to protect them from predators. For example, big cats (lions and tigers) have thick skins and sensitive hearing. The lion-tailed macaque (also called Beard ape) lives in the rainforests of Western Ghats. Its most outstanding feature is the silver-white mane, which surrounds the head from the cheeks down to its chin. It is a good climber and spends a major part of its life on the tree. It feeds mainly on fruits. It also eats seeds, young leaves, stems, flowers and buds. This beard ape also searches for insects under the bark of the trees. Since it is able to get sufficient food on the trees, it rarely comes down on the ground.

Difference between Weather and Climate
Weather and climate appear somewhat same. Right? But still it is a fact that they are quite different. Weather chiefly concerns the present and near-term future state of the atmosphere. Should you wear a jacket? Will it rain tomorrow? Will we go to school tomorrow if this snow continues? Media outlets such as newspapers, radio, and television help you answer these and similar questions by reporting on atmospheric conditions gathered from American government sources.
Weather is the mix of events that happen each day in our atmosphere including temperature, rainfall and humidity. Weather is not the same everywhere.
Climate in your place on the globe controls the weather where you live. Climate is the average weather pattern in a place over many years. So, the climate of Antarctica is quite different than the climate of a tropical island. Hot summer days are quite typical of climates in many regions of the world, even without the effects of global warming.
Climates are changing because our Earth is warming, according to the research of scientists. Does this contribute to a warm summer day? It may, however global climate change is actually much more complicated than that because a change in the temperature can cause changes in other weather elements such as clouds or precipitation.

Global Warming

We frequently hear the term Global warming around us. Although most of us are quite familiar with it, still we are not too serious with it and take it lightly. But it is not that easy to undergo. It is attempting too destroy our mother Earth. It is recognised that Global Warming is essential for our survival, but till a limited scale only.  It is going above that limit and is expected to increase the global temperature to a level that is unmanageable in coming years. Let me help you recall that Global Warming is the average increase in global warming due to emission of greenhouse gases.

A warming planet thus leads to a change in climate which can affect weather in various ways.  Many of these greenhouse gases are actually life-enabling, for without them, heat would escape back into space and the Earth’s average temperature would be a lot colder.

However, if the greenhouse effect becomes stronger, then more heat gets trapped than needed, and the Earth might become less habitable for humans, plants and animals.

Carbon dioxide, though not the most potent of greenhouse gases, is the most significant one. Human activity has caused an imbalance in the natural cycle of the greenhouse effect and related processes. NASA’s Earth Observatory is worth quoting the effect human activity is having on the natural carbon cycle.

Is Global Warming cooler than expected?

Several leading authorities on climate change have given a guarded welcome to research suggesting the Earth may warm more slowly than scientists had expected.

The Earth is now warming faster than at any time in the last 11,000 years, but scientists do not understand clearly why the atmosphere has warmed less than they expected over the last decade or so – and more slowly than in the 1990s.

The researchers looked at how the last decade would affect the long-term sensitivity of the climate to a doubling of atmospheric concentrations of carbon dioxide and suggest the Earth will warm more slowly than expected this century.

But even though the heating may be slower, giving politicians more time to act, the scientists still believe temperatures will eventually climb to 4°C above pre-industrial levels, well above danger levels.

The study should certainly be taken very seriously, although we will need to see over the next year or two how well it stands up to scrutiny.

Does anyone show concern for Earth to decrease Global Warming?

On World Earth Day, there were many residents in the city of Ludhiana, India who confused it with earth hour, but they showed their deep concern over the fading green cover, global warming and many such environmental issues which needed immediate attention. Bringing greenery to society should be the main aim of an individual.

Global warming is the burning issue and we should avoid using such things that increases the amount of dangerous gases and particles in the environment. Like students are fined in their school, people should be made to pay earth tax if they make the environment dirty.

India’s Weather and Climate
The overall weather is mainly hot most of the year with significant variations from region to region. The coolest weather lasts from around the end of November to the beginning of March, with fresh mornings and evenings, and mostly sunny days. The really hot weather, when it is dry, dusty and unpleasant, is between March and June. Monsoon rains occur in most regions in summer anywhere between June and early October.
Western Himalayas including Srinagar is best from March to October; July to August can be cold and damp in winter. Shimla is higher and therefore colder in winter. Places like Gulmarg, Manali and Pahalgam are usually under several feet of snow from December to March and temperatures in Ladakh, which is a high-altitude desert, can be extremely cold. The mountain passes of Ladakh are accessible from July to October.
Our northern plains that consist cities like New Delhi, Varanasi, Lucknow and Patna experience an extreme range of temperatures and are typically warm from April to mid-June, falling to almost freezing at night in winter between November and February. Summers are hot with monsoons between June and September.
In the centre, Madhya Pradesh state escapes the very worst of the hot season, but monsoons are heavy between July and September. Temperatures fall at night in winter.
Western India has November to February as most comfortable months, although evenings can be fairly cold. In a possibility, summers can be extremely hot with monsoon rainfall between mid June and mid September.
Towards the eastern India the weather in states like Orissa (which is flood-prone) are defined by cooler weather from October to February, scorching heat from March to May and unavoidable drenching from the monsoons from June to October.
In our southwest, the most pleasant weather is from November to March. Monsoon rains fall anywhere between late April and July. Summer temperatures are not as high as Northern India although humidity is extreme. The coast benefits from some cooling breezes. Inland, Mysore and Bijapur have pleasant climates with relatively low rainfall.

In the southeast, Tamil Nadu experiences a northeast monsoon between October and December and temperatures and humidity are

high all year. The hills can be cold in winter.

In the northeast, March to June and September to November are the driest and most pleasant periods. The rest of the year has extremely heavy monsoon rainfall.

Climate of Brazil

There are four seasons in Brazil, though only the southern area experiences any true change between the four. Other areas of the country experience two main seasons: the dry and the rainy seasons.
The times of the seasons are the exact opposite of Europe and the US, with winter beginning the 22nd of June and summer starting on December 22nd. Spring begins in September and autumn's first day is the 22nd of March.
The rainy season will begin in the autumn for parts of the Amazon and not until winter in other areas, but it will last about six months for all of the rainforest.
Other parts of Brazil are more agreeable year-round, especially the northeast and the area around Rio de Janeiro. Showers do come up unexpectedly, which can ruin a tourist's day at the beach, but that is just part of the experience of visiting Brazil.
The southern region of Brazil can be quite cold in the winter. Light coats and sweaters are needed when the temperatures dip down to 41F or 5C. This past June saw record lows for many of the small towns and even some snow in areas.
Climate of USA
The Climate of the United States varies due to its positioning of states in latitude, and range of geographic features. West of the 100th meridian, much of the U.S. is semi-arid to desert in the far south western U.S. To the east of the 100th meridian, the climate is humid continental in the northern areas (locations above 40 north latitude), to humid temperate in the central and Atlantic coast regions, to humid subtropical in the Gulf and south Atlantic regions. The southern tip of Florida is tropical. Much of the Rocky Mountains, the Sierra Nevada, and the Cascade Range are alpine. The climate along the coast of California is Mediterranean, while the upper West coast is areas in coastal Oregon and Washington are cool temperate oceanic. The state of Alaska—on the north-western corner of the North American continent—is largely subarctic, with an oceanic climate in its southern edge and a polar climate in the north. The archipelago state of Hawaii, in the middle of the Pacific Ocean, is tropical.

Like most landmasses located in the middle and lower middle latitudes, the primary driver of weather in the contiguous United States is the seasonal change in the solar angle and the polar jet stream. In the northern hemisphere summer, the oceanic subtropical high pressure systems move north - and much of the central and southern U.S. see stable weather, sunshine, and warm to hot temperatures. In the Northern Hemispheric winter, the subtropical highs retreat southward and the polar front jet stream moves further south into the United States - bringing much greater weather variation and much warmer temperature. Areas in the extreme southern U.S., like Florida, the Gulf Coast, the Desert Southwest, and southern California, however, often have more stable weather as the polar jet stream’s impact often does not reach that far south.

Mobile weather systems are more active in the winter or colder months than in the summer or in other words warmer months in the United States. In the winter months, storms come from the Pacific Ocean and enter the U.S. through the Pacific Northwest, then move out across the Great Plains, then move eastward off the central and northern Atlantic seaboard. In the summer months, storms are much more localized (short duration thunderstorms are common in many areas east of the 100th meridian) and large scale storms are much less frequent and the duration is much shorter. In late summer and fall, tropical cyclones infrequently move toward the Gulf and south Atlantic states, bringing high winds, heavy rainfall, and tidal surges to the coastal plain.

Climate of Africa

The climate of Africa ranges from tropical to subarctic on its highest peaks. Its northern half is primarily desert or arid, while its central and southern areas contain both savanna plains and very dense jungle (rainforest) regions. In between, there is a convergence where vegetation patterns such as Sahel and steppe dominate. The movement of the Inter-tropical convergence zone, also known as the monsoon trough, creates a rainy season across central portions of the continent to the south of the Sahara. Tropical waves moving offshore Africa caused by the African easterly jet lead to many of the northern Atlantic's tropical cyclones annually. The Sahara is the hottest and driest portion of Africa due to the presence of the subtropical ridge.

Globally, heating of the earth near the equator leads to large amounts of upward motion and convection along the monsoon trough or Inter-tropical convergence zone. The divergence over the near-equatorial trough leads to air rising and moving away from the equator aloft. As it moves towards the Mid-Latitudes, the air cools and sinks, which leads to subsidence near the 30th parallel of both hemispheres. This circulation is known as the Hadley cell and leads to the formation of the subtropical ridge. Many of the world's deserts are caused by these climatologically high-pressure areas, including the Sahara.

Climate of Australia

The climate of Australia varies widely due to its large geographical size, but by far the largest part of Australia is desert or semi-arid. Only the south-east and south-west corners have a temperate climate and moderately fertile soil. The northern part of the country has a tropical climate, varied between tropical rainforests, grasslands, part desert.
Australia's climate is ruled by the hot, sinking air of the subtropical high pressure belt which moves north and south with the seasons. This causes the rainfall pattern over Australia to be highly seasonal. Australia's rainfall is the lowest of the seven continents (besides Antarctica). Rainfall is variable, with frequent droughts lasting several seasons.
Since it is a small continent separated from Polar Regions by the Southern Ocean, Australia does not get the harsh snaps of polar air that swarm over Northern Hemisphere continents during winter. The continents in the Northern Hemisphere have a considerable temperature contrast between summer and winter, whereas in Australia the temperature contrast is small. In many parts of the country, seasonal high and lows can be great with temperatures ranging from above 50 °C (122 °F) to well below zero. Minimum temperatures are moderated by the lack of mountains and the influence of surrounding oceans.

Forecasting weather and predicting climate
Weather forecasters try to answer questions like: What will the temperature be tomorrow? Will it rain? How much rain will we have? Will there be thunderstorms? Today, most weather forecasts are based on models, which incorporate observations of air pressure, temperature, humidity and winds to produce the best estimate of current and future conditions in the atmosphere. A weather forecaster then looks at the model output to figure out the most likely scenario.  The accuracy of weather forecasts depend on both the model and on the forecaster’s skill. Short-term weather forecasts are accurate for up to a week.
Climate predictions take a much longer-term view.  These predictions try to answer questions like how much warmer will the Earth be 50 to 100 years from now? How much more precipitation will there be? How much will sea level rise? Climate predictions are made using global climate models. Unlike weather forecast models, climate models cannot use observations because there are no observations in the future.

May be it is difficult to understand  but let me tell you, our Rig-Veda, which is the oldest Veda ever found in India, mentioned methods to calculate everyday temperature very accurately to an exact point. But these were very complex calculations and that today’s scientists cannot do it because they are unaware of these concepts. During that period almost every person could find the everyday temperature quite easily.

Causes of Global Warming

The Earth's climate is fueled by the Sun. Most of the Sun's energy, called solar radiation, is absorbed by the Earth, but some is reflected back into space. A natural layer of atmospheric gases absorbs a portion of this reflected solar radiation, eventually releasing some of it into space, but forcing much of it back to Earth. There it warms the Earth's surface creating what is known as the natural "greenhouse effect," as illustrated in the diagram below.

Without the natural greenhouse effect, the Earth's average temperature would be much colder, and the planet would be covered with ice.

Recent scientific evidence shows that the greenhouse effect is being increased by release of certain gases to the atmosphere that cause the Earth's temperature to rise. This is called "global warming." Carbon dioxide (CO2) accounts for about 85 percent of greenhouse gases released in the U.S. CO2 emissions are largely due to the combustion of fossil fuels in electric power generation. Methane (CH4) emissions, which result from agricultural activities, landfills, and other sources, are the second largest contributor to greenhouse gases in the U.S.

Industrial applications such as foam production, refrigeration, dry cleaning, chemical manufacturing, and semiconductor manufacturing produce other greenhouse gas emissions such as hydro fluorocarbons (HFCs). Smelting of aluminium produces another greenhouse gas called per fluorinated compounds (PFCs). Emissions of NOx and VOC from automobile exhaust and industrial processes contribute to the formation of ground-level ozone or smog, also a greenhouse gas.

अब हमें यह ज्ञात हो चूका हैं  की ग्लोबल वार्मिंग हमारे हेतु कितनी विशाल समस्या हैं । इसके अतिरिक्त फैलता प्रदूषण  पृथ्वी के मौसम और जलवायु पर बुरा प्रभाव  दल रहा है । हमें यह भली भांति जानना चाहिए  की यदि हम  जल्द ही  कुछ  नहीं करते तो इसका हमारे ऊपर बहुत बुरा प्रभाव पर सकता है ।  हमें प्रयास करना चाहिए की हम  कम से कम ग्रीन हाउस गैसों का  उत्सर्जन 
करे । जब हम गाड़ी की अथवा स्कूटर की सवारी करते  हैं तब हम वातावरण दूषित करने में  अपना योगदान देते हैं । अर्थात यदि हम  अबी भी सतर्क नहीं हुए तो पीड़ा अत्यधिक हो जाएगी । इस स्तिथि में हमारा प्रयास ही हमारी सहायता करने योग्य है । अगर हम न्यूनतम मात्रा में अपनी नदियों को प्रदूषित करे, ग्रीन हाउस गैसों का वीर्यपात करे, उत्तम मात्रा में वृक्ष उगाए आदि। अंत में मैं आप सबसे गुज़ारिश करती हूँ  कि अपनी धरती माँ की देनों का तिरस्कार न  करते हुए मौसम और जलवायु का सही प्रकार से ध्यान रखें ।  अन्यथा हमारी यह कृत अनर्थकारी सिद्ध हो सकता है ।