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Guru Granth Sahib
Composition, Arrangement & Layout
ਜਪੁ | Jup
ਸੋ ਦਰੁ | So Dar
ਸੋਹਿਲਾ | Sohilaa
ਰਾਗੁ ਸਿਰੀਰਾਗੁ | Raag Siree-Raag
Gurbani (14-53)
Ashtpadiyan (53-71)
Gurbani (71-74)
Pahre (74-78)
Chhant (78-81)
Vanjara (81-82)
Vaar Siri Raag (83-91)
Bhagat Bani (91-93)
ਰਾਗੁ ਮਾਝ | Raag Maajh
Gurbani (94-109)
Ashtpadi (109)
Ashtpadiyan (110-129)
Ashtpadi (129-130)
Ashtpadiyan (130-133)
Bara Maha (133-136)
Din Raen (136-137)
Vaar Maajh Ki (137-150)
ਰਾਗੁ ਗਉੜੀ | Raag Gauree
Gurbani (151-185)
Quartets/Couplets (185-220)
Ashtpadiyan (220-234)
Karhalei (234-235)
Ashtpadiyan (235-242)
Chhant (242-249)
Baavan Akhari (250-262)
Sukhmani (262-296)
Thittee (296-300)
Gauree kii Vaar (300-323)
Gurbani (323-330)
Ashtpadiyan (330-340)
Baavan Akhari (340-343)
Thintteen (343-344)
Vaar Kabir (344-345)
Bhagat Bani (345-346)
ਰਾਗੁ ਆਸਾ | Raag Aasaa
Gurbani (347-348)
Chaupaday (348-364)
Panchpadde (364-365)
Kaafee (365-409)
Aasaavaree (409-411)
Ashtpadiyan (411-432)
Patee (432-435)
Chhant (435-462)
Vaar Aasaa (462-475)
Bhagat Bani (475-488)
ਰਾਗੁ ਗੂਜਰੀ | Raag Goojaree
Gurbani (489-503)
Ashtpadiyan (503-508)
Vaar Gujari (508-517)
Vaar Gujari (517-526)
ਰਾਗੁ ਦੇਵਗੰਧਾਰੀ | Raag Dayv-Gandhaaree
Gurbani (527-536)
ਰਾਗੁ ਬਿਹਾਗੜਾ | Raag Bihaagraa
Gurbani (537-556)
Chhant (538-548)
Vaar Bihaagraa (548-556)
ਰਾਗੁ ਵਡਹੰਸ | Raag Wadhans
Gurbani (557-564)
Ashtpadiyan (564-565)
Chhant (565-575)
Ghoriaan (575-578)
Alaahaniiaa (578-582)
Vaar Wadhans (582-594)
ਰਾਗੁ ਸੋਰਠਿ | Raag Sorath
Gurbani (595-634)
Asatpadhiya (634-642)
Vaar Sorath (642-659)
ਰਾਗੁ ਧਨਾਸਰੀ | Raag Dhanasaree
Gurbani (660-685)
Astpadhiya (685-687)
Chhant (687-691)
Bhagat Bani (691-695)
ਰਾਗੁ ਜੈਤਸਰੀ | Raag Jaitsree
Gurbani (696-703)
Chhant (703-705)
Vaar Jaitsaree (705-710)
Bhagat Bani (710)
ਰਾਗੁ ਟੋਡੀ | Raag Todee
ਰਾਗੁ ਬੈਰਾੜੀ | Raag Bairaaree
ਰਾਗੁ ਤਿਲੰਗ | Raag Tilang
Gurbani (721-727)
Bhagat Bani (727)
ਰਾਗੁ ਸੂਹੀ | Raag Suhi
Gurbani (728-750)
Ashtpadiyan (750-761)
Kaafee (761-762)
Suchajee (762)
Gunvantee (763)
Chhant (763-785)
Vaar Soohee (785-792)
Bhagat Bani (792-794)
ਰਾਗੁ ਬਿਲਾਵਲੁ | Raag Bilaaval
Gurbani (795-831)
Ashtpadiyan (831-838)
Thitteen (838-840)
Vaar Sat (841-843)
Chhant (843-848)
Vaar Bilaaval (849-855)
Bhagat Bani (855-858)
ਰਾਗੁ ਗੋਂਡ | Raag Gond
Gurbani (859-869)
Ashtpadiyan (869)
Bhagat Bani (870-875)
ਰਾਗੁ ਰਾਮਕਲੀ | Raag Ramkalee
Ashtpadiyan (902-916)
Gurbani (876-902)
Anand (917-922)
Sadd (923-924)
Chhant (924-929)
Dakhnee (929-938)
Sidh Gosat (938-946)
Vaar Ramkalee (947-968)
ਰਾਗੁ ਨਟ ਨਾਰਾਇਨ | Raag Nat Narayan
Gurbani (975-980)
Ashtpadiyan (980-983)
ਰਾਗੁ ਮਾਲੀ ਗਉੜਾ | Raag Maalee Gauraa
Gurbani (984-988)
Bhagat Bani (988)
ਰਾਗੁ ਮਾਰੂ | Raag Maaroo
Gurbani (889-1008)
Ashtpadiyan (1008-1014)
Kaafee (1014-1016)
Ashtpadiyan (1016-1019)
Anjulian (1019-1020)
Solhe (1020-1033)
Dakhni (1033-1043)
ਰਾਗੁ ਤੁਖਾਰੀ | Raag Tukhaari
Bara Maha (1107-1110)
Chhant (1110-1117)
ਰਾਗੁ ਕੇਦਾਰਾ | Raag Kedara
Gurbani (1118-1123)
Bhagat Bani (1123-1124)
ਰਾਗੁ ਭੈਰਉ | Raag Bhairo
Gurbani (1125-1152)
Partaal (1153)
Ashtpadiyan (1153-1167)
ਰਾਗੁ ਬਸੰਤੁ | Raag Basant
Gurbani (1168-1187)
Ashtpadiyan (1187-1193)
Vaar Basant (1193-1196)
ਰਾਗੁ ਸਾਰਗ | Raag Saarag
Gurbani (1197-1200)
Partaal (1200-1231)
Ashtpadiyan (1232-1236)
Chhant (1236-1237)
Vaar Saarang (1237-1253)
ਰਾਗੁ ਮਲਾਰ | Raag Malaar
Gurbani (1254-1293)
Partaal (1265-1273)
Ashtpadiyan (1273-1278)
Chhant (1278)
Vaar Malaar (1278-91)
Bhagat Bani (1292-93)
ਰਾਗੁ ਕਾਨੜਾ | Raag Kaanraa
Gurbani (1294-96)
Partaal (1296-1318)
Ashtpadiyan (1308-1312)
Chhant (1312)
Vaar Kaanraa
Bhagat Bani (1318)
ਰਾਗੁ ਕਲਿਆਨ | Raag Kalyaan
Gurbani (1319-23)
Ashtpadiyan (1323-26)
ਰਾਗੁ ਪ੍ਰਭਾਤੀ | Raag Prabhaatee
Gurbani (1327-1341)
Ashtpadiyan (1342-51)
ਰਾਗੁ ਜੈਜਾਵੰਤੀ | Raag Jaijaiwanti
Gurbani (1352-53)
Salok | Gatha | Phunahe | Chaubole | Swayiye
Sehskritee Mahala 1
Sehskritee Mahala 5
Gaathaa Mahala 5
Phunhay Mahala 5
Chaubolae Mahala 5
Shaloks Bhagat Kabir
Shaloks Sheikh Farid
Swaiyyae Mahala 5
Swaiyyae in Praise of Gurus
Shaloks in Addition To Vaars
Shalok Ninth Mehl
Mundavanee Mehl 5
ਰਾਗ ਮਾਲਾ, Raag Maalaa
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Iceland Volcano Eruption Could Last Months
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<blockquote data-quote="spnadmin" data-source="post: 126936" data-attributes="member: 35"><p><span style="color: Blue"><strong>Story continues</strong></span></p><p></p><p style="text-align: left"><span style="color: Black"><em>Weather Talk</em></span></p> <p style="text-align: left"><em>By Mark Vogan</em></p> <p style="text-align: left"><span style="color: Black"></span></p> <p style="text-align: left"><span style="color: Black"><a href="http://markvoganweather.blogspot.com/2010/04/todays-top-weather-stories-on-weather_16.html" target="_blank">http://markvoganweather.blogspot.com/2010/04/todays-top-weather-stories-on-weather_16.html</a></span></p> <p style="text-align: left"><span style="color: Black"></span></p> <p style="text-align: left"><span style="color: Black"></span> <span style="color: Black">Though Eyjafjallajokull likely won't have weather or climatic influence on a global-scale (FOR NOW ANYWAY), but did this have other "in-direct influences of surface temperature in Britain and Europe the past few days?</span></p> <p style="text-align: left"><span style="color: Black"></span> </p> <p style="text-align: left"><span style="color: black">Though the continuous eruption of the Eyjafjallajokull volcano in southwest Iceland likely won't have impact on either global weather patterns or long-term climate simply because this hasn't produced a powerful enough release into the atmosphere, ash and gasses etc would have needed to be forced upwards and into the stratosphere, some 30,000 feet "higher" than the levels this ash at the moment is reaching (between 20,000-30,000ft) in order to catch the very highest, upper-level atmosphereic winds that circle our world and this would have probably been a much more likely scenario for alterations in global weather and or climatic patterns as like we saw with Mt St Helens in WA, USA were ash fell on the East Coast, thousands of miles from the volcano itself, these gasses and ash clouds reached the very limits of earth's atmosphere, circled the planet and ultimately clouded the worlds outer atmosphere enough to produce several years of cooling... This has happened with many major eruptions such as Pinatubo, Krakatoa and other huge eruptions.. Here is a piece from a Science Fair article released today..</span></p> <p style="text-align: left"></p> <p style="text-align: left"><em>"In 1991, the eruption of Mount Pinatubo in the Philippines, the second-largest eruption of the 20th century (much larger than Eyjafjallajokull), sent a sulfuric acid haze into the stratosphere, reducing global average temperatures about 0.9 degrees Fahrenheit over the next year."</em></p> <p style="text-align: left"></p> <p style="text-align: left"><em>Full article <a href="http://content.usatoday.com/communities/sciencefair/post/2010/04/volcano-spews-clouds-of-uncertainty/1" target="_blank">Here</a></em></p> <p style="text-align: left"></p> <p style="text-align: left">That being said, all this recent activity and the mention that in the past, this very volcano in Iceland reacted like it did now just prior to the eruption of a "larger more dangers" nearby volcano by the name I believe "Katyla".. If that was to occur, then this may be a very different story. Many wonder how long all this chaos will last across the UK and Europe, well it depends on two key elements... The actual volcano itself and it's activity and behavior as well as weather... Which is seeing a jet stream flow from Canada, Greenland and across Iceland, where it's 30,000ft band of winds is picking up the upward flow of ash to the jet level and unfortunately, this jet flow is pushing all this ash cloud into the heart of one of, if not thee busiest airspaces on earth, therefore creating the massive problems. Until this flow changes, we are likely to see continuous issues with flights.</p> <p style="text-align: left"></p> <p style="text-align: left">OK, so what in-direct weather related influences MAY this volcano be having on the ground here in Britain and across Scandinavia, Netherlands, Belgium and other European countries which have their airpspace closed?</p> <p style="text-align: left"></p> <p style="text-align: left">Well. The complete absense of airtraffic over this large area I believe may be allowing "clearer" air and therefore days with high pressure and perhaps less obstruction between the sun, it's rays and the surface of earth may allow warmer daytime temperatures and at night, cooler temperatures than otherwise would be with thousnads of aircraft travelling through European airspace.. When you look into the skies above somewhere like Heathrow or New York airspace on a clear morning before sunrise,you can actually see the man-made cloud formed by the vast amounts of vapor trails, which on one particular morning when waiting for a flight to LA from Newark, I could see an artificial cloud formed purely by airplanes... The shear absense of airplanes over Britain and Europe MUST be having even a slight impact, especially with lack of cloudcover thanks to the high pressure in control.... But this is purely my own speculation and cannot tell for sure, perhaps an article will be written on this very topic in the future.</p><p></p><p>Interestingly. I drove down to Dumfries from Glasgow this morning where the skies were crystal clear and a surprisingly harsh frost was formed... Is this my theory playing out here? Would it have dropped to -2 or -3C had it not been for the lack of aircraft in the sky? Here at my house today, I reached a high of 61 degrees under clear, sunny skies... Wonderful? Is this high pressure cell and dry spell my summers ideas holding? Time will tell.</p></blockquote><p></p>
[QUOTE="spnadmin, post: 126936, member: 35"] [COLOR=Blue][B]Story continues[/B][/COLOR] [LEFT][COLOR=Black][I]Weather Talk[/I][/COLOR] [I]By Mark Vogan[/I] [COLOR=Black] [url]http://markvoganweather.blogspot.com/2010/04/todays-top-weather-stories-on-weather_16.html[/url] [/COLOR] [COLOR=Black]Though Eyjafjallajokull likely won't have weather or climatic influence on a global-scale (FOR NOW ANYWAY), but did this have other "in-direct influences of surface temperature in Britain and Europe the past few days? [/COLOR] [COLOR=black]Though the continuous eruption of the Eyjafjallajokull volcano in southwest Iceland likely won't have impact on either global weather patterns or long-term climate simply because this hasn't produced a powerful enough release into the atmosphere, ash and gasses etc would have needed to be forced upwards and into the stratosphere, some 30,000 feet "higher" than the levels this ash at the moment is reaching (between 20,000-30,000ft) in order to catch the very highest, upper-level atmosphereic winds that circle our world and this would have probably been a much more likely scenario for alterations in global weather and or climatic patterns as like we saw with Mt St Helens in WA, USA were ash fell on the East Coast, thousands of miles from the volcano itself, these gasses and ash clouds reached the very limits of earth's atmosphere, circled the planet and ultimately clouded the worlds outer atmosphere enough to produce several years of cooling... This has happened with many major eruptions such as Pinatubo, Krakatoa and other huge eruptions.. Here is a piece from a Science Fair article released today..[/COLOR] [I]"In 1991, the eruption of Mount Pinatubo in the Philippines, the second-largest eruption of the 20th century (much larger than Eyjafjallajokull), sent a sulfuric acid haze into the stratosphere, reducing global average temperatures about 0.9 degrees Fahrenheit over the next year."[/I] [I]Full article [URL="http://content.usatoday.com/communities/sciencefair/post/2010/04/volcano-spews-clouds-of-uncertainty/1"]Here[/URL][/I] That being said, all this recent activity and the mention that in the past, this very volcano in Iceland reacted like it did now just prior to the eruption of a "larger more dangers" nearby volcano by the name I believe "Katyla".. If that was to occur, then this may be a very different story. Many wonder how long all this chaos will last across the UK and Europe, well it depends on two key elements... The actual volcano itself and it's activity and behavior as well as weather... Which is seeing a jet stream flow from Canada, Greenland and across Iceland, where it's 30,000ft band of winds is picking up the upward flow of ash to the jet level and unfortunately, this jet flow is pushing all this ash cloud into the heart of one of, if not thee busiest airspaces on earth, therefore creating the massive problems. Until this flow changes, we are likely to see continuous issues with flights. OK, so what in-direct weather related influences MAY this volcano be having on the ground here in Britain and across Scandinavia, Netherlands, Belgium and other European countries which have their airpspace closed? Well. The complete absense of airtraffic over this large area I believe may be allowing "clearer" air and therefore days with high pressure and perhaps less obstruction between the sun, it's rays and the surface of earth may allow warmer daytime temperatures and at night, cooler temperatures than otherwise would be with thousnads of aircraft travelling through European airspace.. When you look into the skies above somewhere like Heathrow or New York airspace on a clear morning before sunrise,you can actually see the man-made cloud formed by the vast amounts of vapor trails, which on one particular morning when waiting for a flight to LA from Newark, I could see an artificial cloud formed purely by airplanes... The shear absense of airplanes over Britain and Europe MUST be having even a slight impact, especially with lack of cloudcover thanks to the high pressure in control.... But this is purely my own speculation and cannot tell for sure, perhaps an article will be written on this very topic in the future.[/LEFT] Interestingly. I drove down to Dumfries from Glasgow this morning where the skies were crystal clear and a surprisingly harsh frost was formed... Is this my theory playing out here? Would it have dropped to -2 or -3C had it not been for the lack of aircraft in the sky? Here at my house today, I reached a high of 61 degrees under clear, sunny skies... Wonderful? Is this high pressure cell and dry spell my summers ideas holding? Time will tell. [/QUOTE]
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