BEGIN:VCALENDAR
VERSION:2.0
PRODID:-//jEvents 2.0 for Joomla//EN
CALSCALE:GREGORIAN
METHOD:PUBLISH
BEGIN:VEVENT
UID:8e35730ac3b29aa39baf3e1505c240b5
CATEGORIES:Polar Conferences, Meetings and Events
CREATED:20170519T092959
SUMMARY:Glacial and Periglacial Geomorphology session at the 9th International Conference on Geomorphology
LOCATION:Vigyan Bhawan\, New Delhi
DESCRIPTION:Glacial and Periglacial Geomorphology session at the 9th International Conf
 erence on Geomorphology, 6-11 November, New Delhi, India\n \nThe deadline f
 or registration and abstracts for the upcoming 9th International Conference
  on Geomorphology (9th ICG), which will be held in Vigyan Bhawan, New Delhi
  (India) on 6-11 November 2017, has been postponed to May 20th, 2017.\nYou 
 are encouraged to submit a contribution to the Session S19 - "Glacial and P
 eriglacial Geomorphology" (http://www.icg2017.com/authors_guideline.php (ht
 tp://www.icg2017.com/authors_guideline.php)).\nThe Registration page is ope
 n at: https://tciconferences.eventsair.com/icg2017/icgregistration/Site/Reg
 ister (https://tciconferences.eventsair.com/icg2017/icgregistration/Site/Re
 gister)\nAbstract submission before May 20th 2017: https://tciconferences.e
 ventsair.com/PresentationPortal/icg2017/submitabstract (https://tciconferen
 ces.eventsair.com/PresentationPortal/icg2017/submitabstract)\nDetailed desc
 ription: S 19 - Glacial and Periglacial Geomorphology\nChairs: Carlo BARONI
  (Italy), This email address is being protected from spambots. You need Jav
 aScript enabled to view it.
				document.getElementById('cloak8822e8ab65591
 0701c0568f5ca31bea4').innerHTML = '';
				var prefix = 'ma' + 'il
 ' + 'to';
				var path = 'hr' + 'ef' + '=';
				var addy8822e8ab655910
 701c0568f5ca31bea4 = 'carlo.baroni' + '@';
				a
 ddy8822e8ab655910701c0568f5ca31bea4 = addy8822e8ab655910701c0568f5ca31bea4 
 + 'unipi' + '.' + 'it';
				var addy_text8822e8ab65
 5910701c0568f5ca31bea4 = 'carlo.baroni' + '@' + 
 'unipi' + '.' + 'it';document.getElementById('cloak
 8822e8ab655910701c0568f5ca31bea4').innerHTML += '<a ' + path + '\'' + prefi
 x + ':' + addy8822e8ab655910701c0568f5ca31bea4 + '\'>'+addy_text8822e8ab655
 910701c0568f5ca31bea4+'';
		 &amp; Milap Chand SHARMA (India), This email a
 ddress is being protected from spambots. You need JavaScript enabled to vie
 w it.
				document.getElementById('cloak5449d32f4b1b66031a4259e047d1b127').
 innerHTML = '';
				var prefix = '&#109;a' + 'i&#108;' + '&#116;o';
				var
  path = 'hr' + 'ef' + '=';
				var addy5449d32f4b1b66031a4259e047d1b127 = '
 m&#105;l&#97;p' + '&#64;';
				addy5449d32f4b1b66031a4259e047d1b127 = addy5
 449d32f4b1b66031a4259e047d1b127 + 'jn&#117;' + '&#46;' + '&#97;c' + '&#46;'
  + '&#105;n';
				var addy_text5449d32f4b1b66031a4259e047d1b127 = 'm&#105;l
 &#97;p' + '&#64;' + 'jn&#117;' + '&#46;' + '&#97;c' + '&#46;' + '&#105;n';d
 ocument.getElementById('cloak5449d32f4b1b66031a4259e047d1b127').innerHTML +
 = '<a ' + path + '\'' + prefix + ':' + addy5449d32f4b1b66031a4259e047d1b127
  + '\'>'+addy_text5449d32f4b1b66031a4259e047d1b127+'';
		\nGlacial and peri
 glacial landforms are relevant features concerned with environmental evolut
 ion in regions under cold climates. Landscape analysis furnishes a key tool
  for identifying and understanding the impact of climatic changes in glacia
 l and periglacial environments, very sensitive to past climatic changes and
  to on-going global change. Glacial and periglacial landforms act as proxie
 s for reconstructing the glacial and periglacial response to a changing wor
 ld. Polar and sub-polar regions and mountain areas at different latitudes r
 epresent key areas for detecting the signature of glacial and periglacial h
 istory. A more accurate knowledge of the precise age of major events relate
 d to past glacial changes and to ice-volume variations is required for bett
 er understanding the impact of climate change acting at present or expected
  for the future and for modelling global sea-level variation.\nAt present, 
 polar ice sheets and mountain glaciers cover almost 10% of the Earth's surf
 ace, accounting for a major share of fresh water. Antarctica and Greenland 
 glacial systems extend over 96% of world’s total glacierized area and play 
 a key role in regulating the Earth’s climate, ocean circulation and global 
 sea level. Hindu Kush-Karakoram-Himalayan region known as the "Third Pole" 
 of the Earth, together with other mountain regions, represent the water tow
 ers feeding many perennial rivers, which support more then 2 billion people
  on the Planet.\nPeriglacial processes also influence global hydrology, eco
 systems, and soil carbon storage. Climatic and environmental changes in gla
 cial and periglacial regions cause adaptation through ecological and evolut
 ionary responses by organisms. Glacier- related hazards reinforce the need 
 of creditable research on the impact of glaciers and deglaciation on the so
 ciety. Present ice cover is just about 1/3 of the Last Glacial Maximum, the
  last of many Late Cenozoic glacial cycles, when large portions of the Eart
 h were widely covered by huge ice sheets and ice fields. It is already esta
 blished that Polar Regions, the Himalayas, and other mountain regions also 
 underwent many glacial and inter-glacial cycles. However, the timing and ex
 tent of glaciations seems to have varied both in space and time. A comprehe
 nsive correlation of timings and style of glaciation at regional and global
  scale is still necessary.\nTherefore, a proper understanding of the climat
 e and glacier dynamics is essential for the future development plans within
  a holistic framework.\nThe conference would cover the following Themes: Gl
 acial Dynamics and Mass Balance, Glacial history and past climatic changes,
  Glacial Hydrology, Geospatial Analysis of Glaciers, Periglacial &amp; Para
 glacial Processes, Glacial Lakes &amp; Outburst Floods, Glaciers &amp; Clim
 ate, Glaciers and Society.\n
X-ALT-DESC;FMTTYPE=text/html:<p style="text-align: center;"><strong>Glacial and Periglacial Geomorpholog
 y session at the 9th International Conference on Geomorphology, 6-11 Novemb
 er, New Delhi, India</strong></p><p>&nbsp;</p><p>The deadline for registrat
 ion and abstracts for the upcoming 9th International Conference on Geomorph
 ology (9th ICG), which will be held in Vigyan Bhawan, New Delhi (India) on 
 6-11 November 2017, has been <strong>postponed to May 20th, 2017</strong>.<
 /p><p>You are encouraged to submit a contribution to the Session S19 - "Gla
 cial and Periglacial Geomorphology" (<a href="http://www.icg2017.com/author
 s_guideline.php">http://www.icg2017.com/authors_guideline.php</a>).</p><p>T
 he Registration page is open at: <a href="https://tciconferences.eventsair.
 com/icg2017/icgregistration/Site/Register">https://tciconferences.eventsair
 .com/icg2017/icgregistration/Site/Register</a><br />Abstract submission bef
 ore May 20th 2017: <a href="https://tciconferences.eventsair.com/Presentati
 onPortal/icg2017/submitabstract" target="_blank" rel="noopener noreferrer">
 https://tciconferences.eventsair.com/PresentationPortal/icg2017/submitabstr
 act</a></p><p>Detailed description: S 19 - Glacial and Periglacial Geomorph
 ology</p><p>Chairs: Carlo BARONI (Italy), <span id="cloak8822e8ab655910701c
 0568f5ca31bea4">This email address is being protected from spambots. You ne
 ed JavaScript enabled to view it.</span><script type='text/javascript'>
			
 	document.getElementById('cloak8822e8ab655910701c0568f5ca31bea4').innerHTML
  = '';
				var prefix = '&#109;a' + 'i&#108;' + '&#116;o';
				var path = '
 hr' + 'ef' + '=';
				var addy8822e8ab655910701c0568f5ca31bea4 = 'c&#97;rl&
 #111;.b&#97;r&#111;n&#105;' + '&#64;';
				addy8822e8ab655910701c0568f5ca31
 bea4 = addy8822e8ab655910701c0568f5ca31bea4 + '&#117;n&#105;p&#105;' + '&#4
 6;' + '&#105;t';
				var addy_text8822e8ab655910701c0568f5ca31bea4 = 'c&#97
 ;rl&#111;.b&#97;r&#111;n&#105;' + '&#64;' + '&#117;n&#105;p&#105;' + '&#46;
 ' + '&#105;t';document.getElementById('cloak8822e8ab655910701c0568f5ca31bea
 4').innerHTML += '<a ' + path + '\'' + prefix + ':' + addy8822e8ab655910701
 c0568f5ca31bea4 + '\'>'+addy_text8822e8ab655910701c0568f5ca31bea4+'<\/a>';

 		</script> &amp; Milap Chand SHARMA (India), <span id="cloak5449d32f4b1b66
 031a4259e047d1b127">This email address is being protected from spambots. Yo
 u need JavaScript enabled to view it.</span><script type='text/javascript'>
 
				document.getElementById('cloak5449d32f4b1b66031a4259e047d1b127').inner
 HTML = '';
				var prefix = '&#109;a' + 'i&#108;' + '&#116;o';
				var path
  = 'hr' + 'ef' + '=';
				var addy5449d32f4b1b66031a4259e047d1b127 = 'm&#10
 5;l&#97;p' + '&#64;';
				addy5449d32f4b1b66031a4259e047d1b127 = addy5449d3
 2f4b1b66031a4259e047d1b127 + 'jn&#117;' + '&#46;' + '&#97;c' + '&#46;' + '&
 #105;n';
				var addy_text5449d32f4b1b66031a4259e047d1b127 = 'm&#105;l&#97;
 p' + '&#64;' + 'jn&#117;' + '&#46;' + '&#97;c' + '&#46;' + '&#105;n';docume
 nt.getElementById('cloak5449d32f4b1b66031a4259e047d1b127').innerHTML += '<a
  ' + path + '\'' + prefix + ':' + addy5449d32f4b1b66031a4259e047d1b127 + '\
 '>'+addy_text5449d32f4b1b66031a4259e047d1b127+'<\/a>';
		</script></p><p>Gl
 acial and periglacial landforms are relevant features concerned with enviro
 nmental evolution in regions under cold climates. Landscape analysis furnis
 hes a key tool for identifying and understanding the impact of climatic cha
 nges in glacial and periglacial environments, very sensitive to past climat
 ic changes and to on-going global change. Glacial and periglacial landforms
  act as proxies for reconstructing the glacial and periglacial response to 
 a changing world. Polar and sub-polar regions and mountain areas at differe
 nt latitudes represent key areas for detecting the signature of glacial and
  periglacial history. A more accurate knowledge of the precise age of major
  events related to past glacial changes and to ice-volume variations is req
 uired for better understanding the impact of climate change acting at prese
 nt or expected for the future and for modelling global sea-level variation.
 </p><p>At present, polar ice sheets and mountain glaciers cover almost 10% 
 of the Earth's surface, accounting for a major share of fresh water. Antarc
 tica and Greenland glacial systems extend over 96% of world’s total glacier
 ized area and play a key role in regulating the Earth’s climate, ocean circ
 ulation and global sea level. Hindu Kush-Karakoram-Himalayan region known a
 s the "Third Pole" of the Earth, together with other mountain regions, repr
 esent the water towers feeding many perennial rivers, which support more th
 en 2 billion people on the Planet.</p><p>Periglacial processes also influen
 ce global hydrology, ecosystems, and soil carbon storage. Climatic and envi
 ronmental changes in glacial and periglacial regions cause adaptation throu
 gh ecological and evolutionary responses by organisms. Glacier- related haz
 ards reinforce the need of creditable research on the impact of glaciers an
 d deglaciation on the society. Present ice cover is just about 1/3 of the L
 ast Glacial Maximum, the last of many Late Cenozoic glacial cycles, when la
 rge portions of the Earth were widely covered by huge ice sheets and ice fi
 elds. It is already established that Polar Regions, the Himalayas, and othe
 r mountain regions also underwent many glacial and inter-glacial cycles. Ho
 wever, the timing and extent of glaciations seems to have varied both in sp
 ace and time. A comprehensive correlation of timings and style of glaciatio
 n at regional and global scale is still necessary.</p><p>Therefore, a prope
 r understanding of the climate and glacier dynamics is essential for the fu
 ture development plans within a holistic framework.</p><p>The conference wo
 uld cover the following Themes: Glacial Dynamics and Mass Balance, Glacial 
 history and past climatic changes, Glacial Hydrology, Geospatial Analysis o
 f Glaciers, Periglacial &amp; Paraglacial Processes, Glacial Lakes &amp; Ou
 tburst Floods, Glaciers &amp; Climate, Glaciers and Society.</p>
CONTACT:This email address is being protected from spambots. You need JavaScript enabled to view it.
				document.getElementById('cloakc794f492e8483f66322879347883ce79').innerHTML = '';
				var prefix = '&#109;a' + 'i&#108;' + '&#116;o';
				var path = 'hr' + 'ef' + '=';
				var addyc794f492e8483f66322879347883ce79 = 'c&#97;rl&#111;.b&#97;r&#111;n&#105;' + '&#64;';
				addyc794f492e8483f66322879347883ce79 = addyc794f492e8483f66322879347883ce79 + '&#117;n&#105;p&#105;' + '&#46;' + '&#105;t';
				var addy_textc794f492e8483f66322879347883ce79 = 'c&#97;rl&#111;.b&#97;r&#111;n&#105;' + '&#64;' + '&#117;n&#105;p&#105;' + '&#46;' + '&#105;t';document.getElementById('cloakc794f492e8483f66322879347883ce79').innerHTML += '<a ' + path + '\'' + prefix + ':' + addyc794f492e8483f66322879347883ce79 + '\'>'+addy_textc794f492e8483f66322879347883ce79+'';
		; This email address is being protected from spambots. You need JavaScript enabled to view it.
				document.getElementById('cloak15ac1e9e76f6fe16a3361f8ae9853052').innerHTML = '';
				var prefix = '&#109;a' + 'i&#108;' + '&#116;o';
				var path = 'hr' + 'ef' + '=';
				var addy15ac1e9e76f6fe16a3361f8ae9853052 = 'm&#105;l&#97;p' + '&#64;';
				addy15ac1e9e76f6fe16a3361f8ae9853052 = addy15ac1e9e76f6fe16a3361f8ae9853052 + 'jn&#117;' + '&#46;' + '&#97;c' + '&#46;' + '&#105;n';
				var addy_text15ac1e9e76f6fe16a3361f8ae9853052 = 'm&#105;l&#97;p' + '&#64;' + 'jn&#117;' + '&#46;' + '&#97;c' + '&#46;' + '&#105;n';document.getElementById('cloak15ac1e9e76f6fe16a3361f8ae9853052').innerHTML += '<a ' + path + '\'' + prefix + ':' + addy15ac1e9e76f6fe16a3361f8ae9853052 + '\'>'+addy_text15ac1e9e76f6fe16a3361f8ae9853052+'';
		
DTSTAMP:20260712T160200
DTSTART;TZID=UTC;VALUE=DATE:20171106
DTEND;TZID=UTC;VALUE=DATE:20171112
SEQUENCE:0
TRANSP:OPAQUE
END:VEVENT
END:VCALENDAR