VIJAYAWADA is practically the centre of Andhra in all its aspects. It is an important junction in the Madras-Calcutta, Madras - Delhi routes, and probably the foremost town of Andhra. It contains three ancient temples viz., the Kanakadurga temple, the Malleswaraswamy temple and the Vijayeswaraswami temple. These are the three temples of Vijayawada.
Vijayawada is known in mythology as Vijayavata, and is mentioned in some inscriptions as Rajendracholapura also. it is a famous place of pilgrimage on the river Krishna, and 'has a temple dedicated to Lord Siva in his aspect of Malleswara or Jayasena. Sage Agasthya is said to have been the greatest devotee of this deity and admirer of the deity's several leelas.The origin or installation of Kanaka - durga Devi at Vijayawada is unknown. She is said to be Swayambu or selfmanifest. She also takes the aspect of Chandi or destroyer of the demon Durgama who was causing havoc among the peace - loving inhabitants of Dakshinapatha.
Mallikarjuna or the Malleswara as he is known in the Puranas is said to have been installed by Yudhishthira, the eldest of the Pancha Pandavas, as a token of their victory of the South. Thribhuvana Malla, Western Chalukya King of the 10th century A.D, historically constructed the temple.
The installation of Vijayeswara is said to have been done by Arjuna, one of the Pancha Pandavas, to commemorate his victory with Lord Siva in the shape of Kirata or hunter.
The place Vijayawada is surrounded by many hillocks and the most important of them is Seethanagaram, while the less important is called the Kanakadurga or Kanaka konda. On the southern side of the Kanakadurga temple, is a hillock with sculptures bearing inscriptions, indicating the names of Gods and Goddesses cut below them. Most of these figures are forms of the Goddess in her aspect of Durga, which are dealt with in the Mantra Sastras. Traditionally these hills were originally continuous and at the command of the Lord, they got separated, making enough space for the river Krishna to pass through.
One of these hills is called Indrakila, which is a famous hill mentioned in the Mahabharata as the place where the Pandava hero Arjuna obtained from Lord Siva an important weapon called Pasupatastra. The aspect of Lord Siva who appeared before Arjuna for granting him the boon is Kirata or the hunter. Bharavi in his celebrated Kavya "The Kirtarjuneeya" has immortalized this. The temple of Vijayeswara is attributed to Arjuna to commemorate the event of obtaining Pasupatha. The shrine has the representation of this and many other events of the Mahabharata commemorated in sculpture.
The legend is as follows:
During their wanderings in the forest, the Pancha Pandavas came to Darukavana, where Vedavyasa met them, and told them that one of them should perform Tapascharya in praise of Lord Siva, and obtain from him, the Pasupatastra as a boon, so that they may easily conquer their enemies. Arjuna was chosen for this task and be betook himself to the top of the Indrakila hill (which is said to be the same as the Indrakila hill of Vijayawada) and was performing intense Tapascharya, with his arms upraised, and standing on one foot, and surrounded by the Pancha Agnis or five fires, with four artificial fires around him, and the fifth being the Sun God himself above him. Being pleased with the great Tapascharya of Arjuna, Lord Siva wanted to further test his sincerity, before granting him the desired boon, and therefore took the form of a Kirata or hunter. Parvati also dressed herself as a huntress and the Sivagana of the Lord also came in several disguises. Accompanied by all these, Lord Siva was hunting on the Indrakila bill, driving a wild boar in front of him.
The wild boar came to the side of Arjuna, and Arjuna being a great warrior, took up his bow, and shot it with a single arrow. At the same time, Lord Siva who was following it also shot it with an arrow, and being struck by both the arrows, the boar fell down dead in the middle. Both the Lord and Arjuna claimed the boar as their kill, and a -controversy arose between them, as to whom the boar should belong. Words led to physical quarrel shortly, and the Lord and Arjuna began to wrestle with each other. An experienced and powerful wrestler though he was, Arjuna was no match before the Lord himself, and was soon exhausted. Even in the midst of that desperate struggle, he never lost his one-pointedness of mind and devotion to the Lord.
The wild boar came to the side of Arjuna, and Arjuna being a great warrior, took up his bow, and shot it with a single arrow. At the same time, Lord Siva who was following it also shot it with an arrow, and being struck by both the arrows, the boar fell down dead in the middle. Both the Lord and Arjuna claimed the boar as their kill, and a -controversy arose between them, as to whom the boar should belong. Words led to physical quarrel shortly, and the Lord and Arjuna began to wrestle with each other. An experienced and powerful wrestler though he was, Arjuna was no match before the Lord himself, and was soon exhausted. Even in the midst of that desperate struggle, he never lost his one - pointedness of mind and devotion to the Lord.
To invoke divine aid in his favor, he made a Shivalinga out of the earth, worshipped it, and offered prayers to it. He saw the flowers, with which he worshipped the Linga, as physically falling on the hunter before him and he thereupon realised that the hunter was none other than the Lord himself. The hunter immediately disappeared and the Lord appeared himself before Arjuna, in all his glory. Arjuna prayed to him and his prayer was granted, and Pasupatha was given to him by Lord Siva, As a commemoration of this great event, Arjuna is supposed to have installed the Vijayeswara temple here, in the Indrakila hill.
In the Indrakila there are several rock-cut temples. These were supposed originally to be ancient temples, but during the course of time, they were completely buried under debris. When quarrying for stone and road metal was done, they were revealed, and the rock-out temples were preserved as protected monuments. There is in the temple an excellent stone sculpture, which contains in all its four faces the story of Kiratarjuneeyam.
There are interesting legends about the origin of the Malleswaraswamy temple also. It is stated that, prior to the Kaliyuga, the sage Agasthya had named the Lord at Vijayawada as Jayasena.The Mahabharata hero Arjuna, who was a great wrestler or Mallayoddha, called the Lord as Malleswara. The thus famous Lord Siva so goes the legend, graces with his presence and blesses the town Vijayawada on the banks of the sacred Krishna River.
There is another legend about this in which it is stated that in the Kaliyuga, as early as Saka year 117, there was a king famous on earth by name Madhava Varma. The son, of this Icing once killed by accident the child of a woman who eked her livelihood by selling the fruits of tamarind trees (Intrini-Jeevini). The king, who meted out justice according to the principles of Dharma, sentenced his own son to be banged, in order to uphold the principles of justice. Pleased at this impartial attitude and the adherence to principles of Dharma, of this king, God Malleswara came down and showered gold on him, which brought back to life the deceased prince and the dead child.
Thus the great Lord Malleswara. Established in this world, the name of the great King Madhava Varma. Later on a pious devotee by name Panditharadhya came here, and proclaimed to the world that the devotees of Lord Siva were superior even to the sages. He illustrated the truth of this, by bundling up live, coal in a piece of cloth, with the tender twig of a Sami tree, without burning it. God Malleswara was pleased with it and manifested himself to this devotee. This Lord according to the popular legend, is Mahadeva Malleswara, "the endless one ' the lover of his devotees and worshipping whom the lords of the earth prospered of old".
There is an inscription in the temple, of the 9th century A.D., in the usual Telugu script. The inscription is strangely recorded from bottom upwards. Its purport is to say that a certain Thrikoti Boyi or Trikoti Boyu, the son of Kaliyama-Boy of Pechchevada, set up the pillar as a commemoration of his own fame, in order to secure distinction for his race. The Thrikoti Boyi is identified in the inscription with a Guhyaka Yaksha, who in Dwaparayuga was directed by Indra to direct Arjuna to Indrakila hill, where Arjuna should worship the Lord Siva in order to obtain Pasupatha from him.
Besides being a religious centre, Vijayawada is also the very centre of Andhra culture. The Chalukyas of Kalyani once conquered this place, and the famous Chinese Huin. Tsang had visited this place in 639 A.D. when Buddhism was at its zenith. Vijayawada that is a famous centre of Andhra thus enshrines three important and ancient temples and the temple of Kanakadurga is especially a sacred and powerful one, which attracts a large number of pilgrims even now.
Vijayawada earlier known as Bezawada, is the third largest city in Andhra Pradesh,India located on the banks of the Krishna River and bounded by the Indrakiladri Hills on the West and the Budameru River on the North. Vijayawada literally translates to "The Place of Victory". Its prominence as a major trading and business center has earned it the title of, “The Business Capital ofAndhrapradesh. Situated along the Madras-Howrah and Madras-Delhi Railway route, this is the largest railway junction of the South Central Railway region. The city is in Krishna District, about 282 kilometres (171 mi) from the state capital Hyderabad. The very mention of Vijayawada, first brings to mind delicious mangoes and pickles. Lying in the rich coastal delta of the state, the cuisine of Vijaywada is spicy and deliciously varied.
The discovery of Stone Age Artifacts remains along the banks of the river from Machilipatnam to Nagarjuna Sagar indicates that this area was inhabited at that time.
Vijayawada is also a centre of Andhra culture, and is a religious center. The Chalukyas of Kalyan once conquered this place, and the famous Chinese Xuanzang (Hsuan-tsang) had visited this place in 639 AD when Buddhism was at its zenith in the region. Kings Choda Gangadeva and Ananga Bhimadeva of the Eastern Ganga Dynasty in the 12th century whose capital was in modern Bhubaneswar and who built the Lingaraja temple had re-annexed considerable part of modern Andhra region and marched up to Godavari but could not cross the wide river bed. He established a town 'Vijaya Bahuda' which means 'return after winning' which became known as Vijayawada.
During the British Raj the city experienced significant growth. In particular, the completion of the Prakasam Barrage in 1959, and railway bridge on the Krishna River have helped the region expand its agriculture and commercial base. Vijayawada Railway station is one of the busiest railway junctions in India. The regions around the city have fertile soil and are irrigated by the river Krishna.
Vijayawada is bounded by the Indrakiladri Hills on the west and the Budameru River on the north. The Northern, North-Western, and South-Western parts of the city are covered by a low range of hills, while the Central, South-Western and North-Western parts are covered by rich and fertile agriculture lands with three major irrigation canals. The topography of Vijayawada is flat, with a few small to medium sized hills. The Krishna River runs through the city. These hills are part of the Eastern Ghats cut through by the Krishna river. They have very low elevation compared to the average elevation of the ghats. Three canals originating from the north side of the Prakasham barrage reservoir, Eluru, Bandar and Ryves, run through the city. Vijayawada is the only city in the world with two rivers, Krishna, Budameru, and three canals. Buckingham Canal originates from the south side of the reservoir. Due to the presence of the Krishna river the soil around here is very fertile and cultivated intensively.
The climate is tropical, with hot summers and moderate winters. The peak temperature reaches 49 °C (120 °F) in May-June, while the winter temperature is 17-25 C. The average humidity is 68% and the average annual rainfall is 965 millimetres (38.0 in). Vijayawada gets its rainfall from both the south-west monsoon and north-east monsoon. It's nicknamed "Blazewada" for its scorching summer heat by the Britishers.
The planet is warming, from North Pole to South Pole, and everywhere in between. Globally, the mercury is already up more than 1 degree Fahrenheit (0.8 degree Celsius), and even more in sensitive polar regions. And the effects of rising temperatures aren’t waiting for some far-flung future. They’re happening right now. Signs are appearing all over, and some of them are surprising. The heat is not only melting glaciers and sea ice, it’s also shifting precipitation patterns and setting animals on the move.
Some impacts from increasing temperatures are already happening.
Ice is melting worldwide, especially at the Earth’s poles. This includes mountain glaciers, ice sheets covering West Antarctica and Greenland, and Arctic sea ice.
Researcher Bill Fraser has tracked the decline of the Adélie penguins on Antarctica, where their numbers have fallen from 32,000 breeding pairs to 11,000 in 30 years.
Sea level rise became faster over the last century.
Some butterflies, foxes, and alpine plants have moved farther north or to higher, cooler areas.
Precipitation (rain and snowfall) has increased across the globe, on average.
Spruce bark beetles have boomed in Alaska thanks to 20 years of warm summers. The insects have chewed up 4 million acres of spruce trees.
Other effects could happen later this century, if warming continues.
Sea levels are expected to rise between 7 and 23 inches (18 and 59 centimeters) by the end of the century, and continued melting at the poles could add between 4 and 8 inches (10 to 20 centimeters).
Hurricanes and other storms are likely to become stronger.
Species that depend on one another may become out of sync. For example, plants could bloom earlier than their pollinating insects become active.
Floods and droughts will become more common. Rainfall in Ethiopia, where droughts are already common, could decline by 10 percent over the next 50 years.
Less fresh water will be available. If the Quelccaya ice cap in Peru continues to melt at its current rate, it will be gone by 2100, leaving thousands of people who rely on it for drinking water and electricity without a source of either.
Some diseases will spread, such as malaria carried by mosquitoes.
Ecosystems will change—some species will move farther north or become more successful; others won’t be able to move and could become extinct. Wildlife research scientist Martyn Obbard has found that since the mid-1980s, with less ice on which to live and fish for food, polar bears have gotten considerably skinnier. Polar bear biologist Ian Stirling has found a similar pattern in Hudson Bay. He fears that if sea ice disappears, the polar bears will as well.
For past climate change, see paleoclimatology and geologic temperature record.
Global annual surface temperatures relative to 1951-1980 mean temperatures from GISS. Analysis summarizes satellite measurements 1982 onward, and ship-based analysis from years earlier. Estimated error 95% confidence resulting from incomplete spatial coverage.[1]
Comparison of ground based (blue) and satellite based (red: UAH; green: RSS) records of temperature variations since 1979. Trends plotted since January 1982.
Mean surface temperature change for the period 2000 to 2009 relative to the average temperatures from 1951 to 1980.[2]
Global warming is the increase in the average temperature of Earth's near-surface air and oceans since the mid-20th century and its projected continuation. Global surface temperature increased 0.74 ± 0.18 °C (1.33 ± 0.32 °F) between the start and the end of the 20th century.[3][A] The Intergovernmental Panel on Climate Change (IPCC) concludes that most of the observed temperature increase since the middle of the 20th century was very likely caused by increasing concentrations of greenhouse gases resulting from human activity such as fossil fuel burning and deforestation.[3] The IPCC also concludes that variations in natural phenomena such as solar radiation and volcanic eruptions had a small cooling effect after 1950.[4][5] These basic conclusions have been endorsed by more than 40 scientific societies and academies of science,[B] including all of the national academies of science of the major industrialized countries.[6]
Climate model projections summarized in the latest IPCC report indicate that the global surface temperature is likely to rise a further 1.1 to 6.4 °C (2.0 to 11.5 °F) during the 21st century.[3] The uncertainty in this estimate arises from the use of models with differing sensitivity to greenhouse gas concentrations and the use of differing estimates of future greenhouse gas emissions. Most studies focus on the period leading up to the year 2100. However, warming is expected to continue beyond 2100 even if emissions stop, because of the large heat capacity of the oceans and the long lifetime of carbon dioxide in the atmosphere.[7][8]
An increase in global temperature will cause sea levels to rise and will change the amount and pattern of precipitation, probably including expansion of subtropical deserts.[9] Warming is expected to be strongest in the Arctic and would be associated with continuing retreat of glaciers, permafrost and sea ice. Other likely effects include changes in the frequency and intensity of extreme weather events, species extinctions, and changes in agricultural yields. Warming and related changes will vary from region to region around the globe, though the nature of these regional variations are uncertain.
Political and public debate continues regarding global warming, and what actions to take in response. The available options are mitigation to reduce further emissions; adaptation to reduce the damage caused by warming; and, more speculatively, geoengineering to reverse global warming. Most national governments have signed and ratified the Kyoto Protocol aimed at reducing greenhouse gas emissions.
Temperature changes
Main article: Temperature record
Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The instrumental record and the unsmoothed annual value for 2004 are shown in black.
The most common measure of global warming is the trend in globally averaged temperature near the Earth's surface. Expressed as a linear trend, this temperature rose by 0.74 ± 0.18 °C over the period 1906–2005. The rate of warming over the last half of that period was almost double that for the period as a whole (0.13 ± 0.03 °C per decade, versus 0.07 °C ± 0.02 °C per decade). The urban heat island effect is estimated to account for about 0.002 °C of warming per decade since 1900.[10] Temperatures in the lower troposphere have increased between 0.13 and 0.22 °C (0.22 and 0.4 °F) per decade since 1979, according to satellite temperature measurements. Temperature is believed to have been relatively stable over the one or two thousand years before 1850, with regionally varying fluctuations such as the Medieval Warm Period and the Little Ice Age.[11]
Estimates by NASA's Goddard Institute for Space Studies and the National Climatic Data Center show that 2005 was the warmest year since reliable, widespread instrumental measurements became available in the late 1800s, exceeding the previous record set in 1998 by a few hundredths of a degree.[12][13] Estimates prepared by the World Meteorological Organization and the Climatic Research Unit show 2005 as the second warmest year, behind 1998.[14][15] Temperatures in 1998 were unusually warm because the strongest El Niño in the past century occurred during that year.[16] Global temperature is subject to short-term fluctuations that overlay long term trends and can temporarily mask them. The relative stability in temperature from 2002 to 2009 is consistent with such an episode.[17][18]
Temperature changes vary over the globe. Since 1979, land temperatures have increased about twice as fast as ocean temperatures (0.25 °C per decade against 0.13 °C per decade).[19] Ocean temperatures increase more slowly than land temperatures because of the larger effective heat capacity of the oceans and because the ocean loses more heat by evaporation.[20] The Northern Hemisphere warms faster than the Southern Hemisphere because it has more land and because it has extensive areas of seasonal snow and sea-ice cover subject to ice-albedo feedback. Although more greenhouse gases are emitted in the Northern than Southern Hemisphere this does not contribute to the difference in warming because the major greenhouse gases persist long enough to mix between hemispheres.[21]
The thermal inertia of the oceans and slow responses of other indirect effects mean that climate can take centuries or longer to adjust to changes in forcing. Climate commitment studies indicate that even if greenhouse gases were stabilized at 2000 levels, a further warming of about 0.5 °C (0.9 °F) would still occur.[22]