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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).\n
 The Registration page is open at: <a href="https://tciconferences.eventsair
 .com/icg2017/icgregistration/Site/Register">https://tciconferences.eventsai
 r.com/icg2017/icgregistration/Site/Register</a>\nAbstract submission before
  May 20th 2017: https://tciconferences.eventsair.com/PresentationPortal/icg
 2017/submitabstract\nDetailed description: S 19 - Glacial and Periglacial G
 eomorphology\nChairs: Carlo BARONI (Italy), This email address is being pro
 tected from spambots. You need JavaScript enabled to view it.
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		 &amp; Milap 
 Chand SHARMA (India), This email address is being protected from spambots. 
 You need JavaScript enabled to view it.
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		\nGlacial and periglacial landforms are relevant features c
 oncerned with environmental evolution in regions under cold climates. Lands
 cape analysis furnishes a key tool for identifying and understanding the im
 pact of climatic changes in glacial and periglacial environments, very sens
 itive to past climatic changes and to on-going global change. Glacial and p
 eriglacial landforms act as proxies for reconstructing the glacial and peri
 glacial response to a changing world. Polar and sub-polar regions and mount
 ain areas at different latitudes represent key areas for detecting the sign
 ature of glacial and periglacial history. A more accurate knowledge of the 
 precise age of major events related to past glacial changes and to ice-volu
 me variations is required for better understanding the impact of climate ch
 ange acting at present or expected for the future and for modelling global 
 sea-level variation.\nAt present, polar ice sheets and mountain glaciers co
 ver almost 10% of the Earth's surface, accounting for a major share of fres
 h 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 clim
 ate, ocean circulation and global sea level. Hindu Kush-Karakoram-Himalayan
  region known as the "Third Pole" of the Earth, together with other mountai
 n regions, represent the water towers feeding many perennial rivers, which 
 support more then 2 billion people on the Planet.\nPeriglacial processes al
 so influence global hydrology, ecosystems, and soil carbon storage. Climati
 c and environmental changes in glacial and periglacial regions cause adapta
 tion through ecological and evolutionary responses by organisms. Glacier- r
 elated hazards reinforce the need of creditable research on the impact of g
 laciers and deglaciation on the society. Present ice cover is just about 1/
 3 of the Last Glacial Maximum, the last of many Late Cenozoic glacial cycle
 s, when large portions of the Earth were widely covered by huge ice sheets 
 and ice fields. It is already established that Polar Regions, the Himalayas
 , and other mountain regions also underwent many glacial and inter-glacial 
 cycles. However, the timing and extent of glaciations seems to have varied 
 both in space and time. A comprehensive correlation of timings and style of
  glaciation at regional and global scale is still necessary.\nTherefore, a 
 proper understanding of the climate and glacier dynamics is essential for t
 he future development plans within a holistic framework.\nThe 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.\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="cloaka6899362e5d1dd6150
 008465201a44df">This email address is being protected from spambots. You ne
 ed JavaScript enabled to view it.</span><script type='text/javascript'>
			
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 		</script> &amp; Milap Chand SHARMA (India), <span id="cloakeb5ebaa4559663
 07626c15d34fe648ad">This email address is being protected from spambots. Yo
 u need JavaScript enabled to view it.</span><script type='text/javascript'>
 
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		</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.
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DTSTAMP:20260427T013301Z
DTSTART;TZID=UTC;VALUE=DATE:20171106
DTEND;TZID=UTC;VALUE=DATE:20171112
SEQUENCE:0
TRANSP:OPAQUE
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