സമുദ്രനിരപ്പിന്റെ ഉയർച്ച
സമുദ്രനിരപ്പിന്റെ ഉയർച്ച എന്നത് ലോകത്തിലെ സമുദ്രങ്ങളിലെ ജലത്തിന്റെ വ്യാപ്തത്തിലുണ്ടാകുന്ന വർധനമൂലം ലോകവ്യാപകമായി ശരാശരി സമുദ്രനിരപ്പിലുണ്ടാകുന്ന ഉയർച്ചയാണ്. സമുദ്രങ്ങളിലെ ജലത്തിന്റെ താപീയവികാസവും അല്ലെങ്കിൽ ഐസ്ഷീറ്റുകളും, കരയിലെ ഗ്ലേസിയറുകളും ഉരുകുന്നതും മൂലം സമുദ്രനിരപ്പിലുണ്ടാകുന്ന ഉയർച്ചയ്ക്ക് കാരണമാകുന്നത് ആഗോള കാലാസ്ഥാമാറ്റമാണ്. കടലിലൂടെ ഒഴുകി നടക്കുന്ന ഐസ് ഷെല്ലുകളോ അല്ലെങ്കിൽ ഐസ് ബർഗ്ഗുകളോ ഉരുകുന്നത് സമുദ്രനിരപ്പ് ചെറുതായി മാത്രമേ കുറിക്കുന്നുള്ളൂ.
പ്രത്യേക മേഖലകളിലെ സമുദ്രനിരപ്പിന്റെ ഉയർച്ച ആഗോള ശരാശരിയേക്കാൾ കൂടുതലോ, കുറവോ ആകാം. ഇതിനെ സ്വാധീനിക്കുന്ന പ്രദേശികമായ ഘടകങ്ങളിൽ ടെക്റ്റോണിക് പ്രഭാവങ്ങൾ, കരഭാഗത്തിന്റെ താണുപോകൽ, വേലിയിറക്കം, സമുദ്രജലപ്രവാഹങ്ങൾ, കൊടുങ്കാറ്റുകൾ മുതലായവ സ്വാധീനിക്കാം. [3]
സമുദ്രതീരങ്ങളിലേയും ദ്വീപുകളിലേയും മനുഷ്യന്റെ ജനസംഖ്യയേയും സമുദ്ര ആവാസവ്യവസ്ഥ പോലെയുള്ള പ്രകൃതിദത്തമായ പരിസ്ഥിതിയേയും സമുദ്രനിരപ്പിന്റെ ഉയർച്ചയ്ക്ക് സ്വാധീനിക്കാൻ കഴിയും. [4]
ഇതും കാണുക
തിരുത്തുകകുറിപ്പുകൾ
തിരുത്തുക- ↑ "Climate Change Indicators in the United States: Sea level". United States Environmental Protection Agency. May 2014.
- ↑ "Why the U.S. East Coast could be a major 'hotspot' for rising seas". The Washington Post. 2016.
- ↑ Fischlin; et al., "Section 4.4.9: Oceans and shallow seas – Impacts", in IPCC AR4 WG2 2007 (ed.), Chapter 4: Ecosystems, their Properties, Goods and Services, p. 234, archived from the original on 2017-06-07, retrieved 2017-06-02
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അവലംബം
തിരുത്തുക- Ipcc ar4 wg1 (2007), Solomon, S.; Qin, D.; Manning, M.; Chen, Z.; Marquis, M.; Averyt, K.B.; Tignor, M.; Miller, H.L. (eds.), Climate Change 2007: The Physical Science Basis, Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, Cambridge University Press, ISBN 978-0-521-88009-1
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പരിശീലനക്കുറിപ്പുകൾ Historical Geology എന്ന താളിൽ ലഭ്യമാണ്