Glacial Lake Outburst Floods Early Warning System to save lives and livelihood of the Nepal Himalaya communities: A case Study of Imja Glacial Lake, Nepal 

Author(s):  
Deepak Kc ◽  
Top Khatri ◽  
Rishiram Sharma

<p>Nepal, a mountainous country, is experiencing multiple disasters, majority of which are induced by Climate Change. Erratic rainfall, extremely high temperature during summer, cold waves are some of them. Nepal will experience the impacts of climate change through an increase in temperature, more frequent heat waves and shorter frost durations in the future (5AR IPCC). Nepal is witnessing the increased maximum temperature of 0.56<sup>o</sup>C per decade and the increment of the temperature is even higher in the mountain region (ICIMOD 2019). One of the major impacts of Climate Change among others, is glacier retreat and Glacial Lake Outburst Floods (GLOFS). Nepal has already experienced more than 26 GLOFS (UNDP and ICIMOD 2020), originated both from Nepal and China, Tibet.</p><p>The Imja Glacial Lake is located at 27° 53′ 55“ N latitude, 86° 55’ 20” E longitude and at an altitude of 5010 m in Everest Region of Nepal Himalayas.  Imja was identified during 1960s as a small supra lake, was later expanded to an area of <strong>1.28 Km<sup>2</sup></strong>, <strong>148.9 meter deep</strong>, holding <strong>75.2 million cubic meters </strong>of water in 2014.   Lake lowering by 3.4 metres and establishment of early warning system was done in 2016 by the Government of Nepal and UNDP with the support of Global Environment Facility.  Hydro-met stations & GLOF Sensors in the periphery and downstream  of Imja Lake and automated early warning sirens in six prime settlements in the  downstream of Imja  watershed  linking with  dynamic SMS Alert system along 50 km downstream of Imja Dudh Koshi River have been have been linked with community-based DRM institutions at local government level. This initiative is important for preparedness and response of GLOF Risk Reduction in the Imja Valley, benefitting 71,752 vulnerable people, both local and the tourists visiting the Everest Region of Nepal.</p><p>Early Warning System of Tsho Rolpa Glacial Lake, the biggest Glacial Lake of Nepal is another example in the such system. New inventory of Glacial Lakes has identified 47 critical lakes as priority lakes for GLOF Risk Reduction in Koshi, Gandaki and Karnali basins. In the new context of federal  governance system, the role of federal, province and local government and communities is crucial  for achieving the targets of  Sendai Framework for Disaster Risk Reduction , particularly target “g” and SDGs 11 and 13  through integrating  the targets in the regular planning and   its’ implementation for resilient and Sustainable Development of  Nepal.</p><p><strong>References:</strong></p><p>Glacial lakes and glacial lake outburst floods in Nepal. Kathmandu, ICIMOD 2011,  Nepal Disaster Report, Ministry of Home affairs (MoHA) , 2015, 2018 Annual Reports UNDP 2016, 2017 and 2018,  Imja Hydro-Meteorological and Early Warning System User Manual, Government of Nepal and UNDP, 2017 Project Completion Report: Community Based Flood and Glacial Lake Outburst Risk Reduction Project, Government of Nepal and UNDP, 2017,  Inventory of glacial lakes and identification of potentially dangerous glacial lakes in the Koshi, Gandaki, and Karnali River Basins of Nepal, the Tibet Autonomous Region of China, and India. Research Report, ICIMOD and UNDP, 2020</p><p> </p>

2015 ◽  
Vol 3 (2) ◽  
pp. 131
Author(s):  
Tiara Sartika Worowirasmi ◽  
Miun Edi Waluyo ◽  
Yuliana Rachmawati ◽  
Itsna Yuni Hidayati

<p class="Abstract"><em>Pertumbuhan penduduk di Kota Semarang yang terus meningkat </em><em>menyebabkan peningkatan kebutuhan lahan </em><em>untuk pemukiman. Keterbatasan lahan dan </em><em>lemahnya </em><em>penegakan peraturan </em><em>atas</em><em> kepemilikan lahan memicu perubahan penggunaan lahan termasuk perubahan penggunaan lahan di daerah aliran sungai. Rencana Tata Ruang Wilayah Kota Semarang tahun 2011-2031 </em><em>menyebutkan bahwa</em><em> DAS Beringin </em><em>merupakan </em><em>daerah penyangga dengan alokasi pembangunan fisik yang dibatasi</em><em>. </em><em>Akan tetapi saat ini warga memanfaatkan DAS sebagai permukiman. Perkembangan pe</em><em>r</em><em>mukiman di DAS mengurangi kemampuan DAS untuk menangkap air dan juga mengurangi kapasitas sungai karena meningkatnya sedimentasi. Kedua hal tersebut adalah penyebab utama dari adanya bencana banjir bandang (yang biasanya terjadi di musim hujan) di tujuh kelurahan yang ada di DAS Beringin. Kondisi ini diperparah dengan banjir rob yang terjadi di dua kelurahan yang terletak di pesisir. Pada </em><em>tahun </em><em>2012, pemerintah Kota Semarang mengembangkan Sistem Peramalan dan Peringatan Banjir sebagai salah satu Upaya Adaptasi Perubahan Iklim yang dikenal sebagai </em>Flood Early Warning System<em> (FEWS). Salah satu output penting dari FEWS adalah pengurangan r</em><em>e</em><em>siko bencana berbasis masyarakat. Proses partisipasi masyarakat dalam FEWS telah memungkinkan masyarakat untuk mengidentifikasi karakteristik r</em><em>e</em><em>siko bencana, mengusulkan solusi untuk mengurangi r</em><em>e</em><em>siko banjir yang sesuai dengan kearifan lokal, meningkatkan kapasitas masyarakat dan mengatur diri mereka sendiri </em><em>melalui </em><em>kelompok siaga bencana </em><em>secara</em><em> mandiri.</em><em></em></p>


Water ◽  
2021 ◽  
Vol 13 (10) ◽  
pp. 1376
Author(s):  
Taigang Zhang ◽  
Weicai Wang ◽  
Tanguang Gao ◽  
Baosheng An

A glacial lake outburst flood (GLOF) is a typical glacier-related hazard in high mountain regions. In recent decades, glacial lakes in the Himalayas have expanded rapidly due to climate warming and glacial retreat. Some of these lakes are unstable, and may suddenly burst under different triggering factors, thus draining large amounts of water and impacting downstream social and economic development. Glacial lakes in the Poiqu River basin, Central Himalayas, have attracted great attention since GLOFs originating there could have a transboundary impact on both China and Nepal, as occurred during the Cirenmaco GLOF in 1981 and the Gongbatongshaco GLOF in 2016. Based on previous studies of this basin, we selected seven very high-risk moraine-dammed lakes (Gangxico, Galongco, Jialongco, Cirenmaco, Taraco, Beihu, and Cawuqudenco) to simulate GLOF propagation at different drainage percentage scenarios (i.e., 25%, 50%, 75%, and 100%), and to conduct hazard assessment. The results show that, when any glacial lake is drained completely or partly, most of the floods will enter Nepal after raging in China, and will continue to cause damage. In summary, 57.5 km of roads, 754 buildings, 3.3 km2 of farmland, and 25 bridges are at risk of damage due to GLOFs. The potentially inundated area within the Chinese part of the Poiqu River basin exceeds 45 km2. Due to the destructive impacts of GLOFs on downstream areas, appropriate and effective measures should be implemented to adapt to GLOF risk. We finally present a paradigm for conducting hazard assessment and risk management. It uses only freely available data and thus is easy to apply.


2018 ◽  
pp. 187-200 ◽  
Author(s):  
Javier Fluixá-Sanmartín ◽  
Javier García Hernández ◽  
Christian Huggel ◽  
Holger Frey ◽  
Alejo Cochachin Rapre ◽  
...  

2021 ◽  
Author(s):  
Joanne Wood ◽  
Stephan Harrison ◽  
Ryan Wilson ◽  
Neil Glasser ◽  
John Reynolds ◽  
...  

&lt;p&gt;Climate change is resulting in mass loss and the retreat of glaciers in the Andes, exposing steep valley sides, over-deepened valley bottoms, and creating glacial lakes behind moraine dams. Glacial Lake Outburst Floods (GLOFs) present the biggest risk posed by glacier recession in Peru. Understanding the characteristics of lakes that have failed in the past will provide an aid to identifying those lakes that might fail in the future and narrow down which lakes are of greatest interest for reducing the risks to local vulnerable populations.&amp;#160;&lt;/p&gt;&lt;p&gt;Using a newly created lake inventory for the Peruvian Andes (Wood et al., in review) and a comprehensive GLOF inventory (unpublished) we investigate lakes from which GLOFs have occurred in the past. This is to establish which physical components of the glacial lake systems are common to those lakes that have failed previously and which can be identified remotely, easily and objectively, in order to improve existing methods of hazard assessment.&lt;/p&gt;


2019 ◽  
Author(s):  
D. Shakya ◽  
V. R. Khadgi ◽  
N. Bajracharya ◽  
S. R. Bajracharya ◽  
S. K. Rai ◽  
...  

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