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Mehta, Manish
- Monitoring of Glacier Changes and Response Time in Chorabari Glacier, Central Himalaya, Garhwal, India
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Authors
Affiliations
1 Centre for Glaciology, Wadia Institute of Himalayan Geology, Dehra Dun 248 001, IN
1 Centre for Glaciology, Wadia Institute of Himalayan Geology, Dehra Dun 248 001, IN
Source
Current Science, Vol 107, No 2 (2014), Pagination: 281-289Abstract
Chorabari Glacier (6.6 sq. km) in the Mandakini River basin, a tributary of the River Alaknanda, Central Himalaya, Garhwal (India) has been monitored in terms of its length and frontal area (snout) changes for the period between 1962 and 2012. Global Positioning System, Survey of India toposheet (1 : 50,000) and ground-based measurements were used to obtain the changes in morphology and size of the glacier. The result shows that the frontal area of the glacier has shrunk by 1% and 344 ± 24 m length loss, with an average rate of 6.8 ± 0.5 m a-1 from 1962 to 2012. The observed terminus records of Chorabari Glacier indicate that the positive mass balance can cause terminus advance in about a 17-year timescale. The lag time of glacier signal transferred from accumulation area to the snout by glacier flow is about 562 years. These observations as well as other studies carried out in the region show a significant reduction in glacier area. The increased retreat rate of the glacier snout is probably a direct consequence of global warming.Keywords
Frontal Areas, Glacier Change, Mass Balance, Response Time, Snout Retreat.- New Occurrence of Albitite from Nubra Valley, Ladakh:Characterization from Mineralogy and Whole Rock Geochemistry
Abstract Views :198 |
PDF Views:76
Authors
Aditya Kharya
1,
H. K. Sachan
1,
Sameer K. Tiwari
1,
Saurabh Singhal
1,
P. Chandra Singh
1,
Santosh Rai
1,
Sushil Kumar
1,
Manish Mehta
1,
P. K. R. Gautam
1
Affiliations
1 Wadia Institute of Himalayan Geology, Dehra Dun 248 001, IN
1 Wadia Institute of Himalayan Geology, Dehra Dun 248 001, IN
Source
Current Science, Vol 111, No 9 (2016), Pagination: 1531-1535Abstract
We report here the occurrence of albitite in Nubra valley of Ladakh region in the Trans-Himalaya area within Indian Territory at 344446N and 77338E before Panamik (in the Wish Pond, local name of the area). The albitite has been characterized by petrography, mineral chemistry, X-ray diffraction and whole rock geochemistry (i.e. major, trace and rare earth elements (REE)). The albitite comprises 85-96% albite and amphibole, whereas apatite, zircon and ilmenite occur as accessory minerals. The textural relationship and geochemical data indicate its igneous origin. The albitite contains about 5-6 ppm U and Th which may possibly host U-REE mineralization.Keywords
Albitite, Karakoram, Mineral Chemistry, XRD, Whole Rock Chemistry.References
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- Modelling of Meteorological Parameters for the Chorabari Glacier Valley, Central Himalaya, India
Abstract Views :226 |
PDF Views:72
Authors
Affiliations
1 Centre for Glaciology, Wadia Institute of Himalayan Geology, Dehradun 248 001, IN
2 Wadia Institute of Himalayan Geology, Dehradun 248 001, IN
1 Centre for Glaciology, Wadia Institute of Himalayan Geology, Dehradun 248 001, IN
2 Wadia Institute of Himalayan Geology, Dehradun 248 001, IN
Source
Current Science, Vol 112, No 07 (2017), Pagination: 1553-1560Abstract
In the present study, we have developed empirical relationships to estimate meteorological parameters at the glacier altitude from the data on non-glacier altitude. Meteorological data collected from automatic weather station at Chorabari Glacier from November 2011 to May 2013 are analysed and empirical equations for air temperature, relative humidity and incoming global radiation are proposed. The dataset of one year (November 2011-October 2012) is used in the calibration of models, while data for the next seven months (November 2012-May 2013) are employed to validate the models. Moreover, an analytical study is also conducted on incoming diffuse radiation (estimated through the established model for India). Further, a relationship is established to correlate the diffuse component of two sites. Variation trend of meteorological parameters with altitude is found to be different for each of the parameters, viz. quadratic for air temperature, logarithmic for relative humidity, and linear for global and diffuse radiation. Performance of the generated equations is tested through various statistical methods. The study reveals that developed correlations are able to give a good match with in situ measurements.Keywords
Clearness Index, Empirical Models, Global and Diffuse Radiation, Meteorology.References
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- Karakoti, I., Kesarwani, K., Mehta, M. and Dobhal, D. P., Extended T-index models for glacier surface melting. Theor. Appl. Climatol., 2016; doi:10.1007/s00704-016-1753-6.
- Mehta, M., Dobhal, D. P., Kesarwani, K., Pratap, B., Kumar, A. and Verma, A., Monitoring of glacier changes and response time in Chorabari Glacier, Central Himalaya, Garhwal, India. Curr. Sci., 2014, 107(2), 281–289.
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- Kesarwani, K., Dobhal, D. P., Durgapal, A. and Mehta, M., High altitude meteorology and cloud cover conditions: a study from Chorabari glacier catchment, Central Himalaya, India. Himalayan Geol., 2015, 36(2), 134–142.
- Kesarwani, K., Dobhal, D. P., Durgapal, A., Karakoti, I. and Mehta, M., Surface energy and mass balance on the ablation zone of Chorabari Glacier, Central Himalaya, India. In Geostatistical and Geospatial Approaches for the Characterization of Natural Resources in the Environment: Challenges, Processes and Strategies (ed. Raju, N. J.), Springer, 2016, pp. 881–885; doi:10.1007/978-3-319-18663-4_136.
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- Das, S. K., Dobhal, D. P. and Juyal, N., Variability of aerosol optical depth and recent recessional trend in Dokriani Glacier, Bhagirathi Valley, Garhwal Himalaya. Curr. Sci., 2010, 99(12), 1816–1821.
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- Mehta, M., Majeed, Z., Dobhal, D. P. and Srivastava, P., Geomorphological evidences of post-LGM glacial advancements in the Himalaya: a study from Chorabari Glacier, Garhwal Himalaya, India. J. Earth Syst. Sci., 2012, 121(1), 149–163.
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- Dobhal, D. P., Mehta, M. and Srivastava, D., Influence of debris cover on terminus retreat and mass changes of Chorabari Glacier, Garhwal region, central Himalaya, India. J. Glaciol., 2013, 59(217), 961–971; doi:10.3189/2013JoG12J180.
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- Enhancement the Gain of Micro Strip Patch Antenna Using Array Configuration Technique
Abstract Views :151 |
PDF Views:4
Authors
Neeraj Rani
1,
Manish Mehta
1
Affiliations
1 Jan Nayak Ch. Devi Lal College of Engineering and Technology, Sirsa, Haryana, IN
1 Jan Nayak Ch. Devi Lal College of Engineering and Technology, Sirsa, Haryana, IN
Source
International Journal of Innovative Research and Development, Vol 5, No 9 (2016), Pagination: 186-191Abstract
A method to enhance the gain of micro strip patch antenna is investigated by array configuration technique. Array configuration technique improves the gain of micro strip patch antenna by increasing the effective aperture area. The effect of array configuration technique in different configurations has been studied numerically and validated experimentally. It is observed that with increase in effective aperture area, the gain of micro strip patch antenna is increased. A technique to increase the effective aperture area is place a number of patches on single dielectric substrate. Compared to single patch antenna, a double patch antenna provides high gain.
Keywords
Micro Strip Patch Antenna, Array, Gain, Return Loss.- Causes and Consequences of Rishiganga Flash Flood, Nanda Devi Biosphere Reserve, Central Himalaya, India
Abstract Views :177 |
PDF Views:88
Authors
Affiliations
1 Wadia Institute of Himalayan Geology, Dehradun 248 001, IN
1 Wadia Institute of Himalayan Geology, Dehradun 248 001, IN
Source
Current Science, Vol 121, No 11 (2021), Pagination: 1483-1487Abstract
On 7 February 2021 at 10:30 am, a huge amount of slurry material flooded the Rishiganga catchment, resulting in excessive flow along the valley. The main cause of this flood was the dislocation of a huge rock mass approximately 540 m wide and 720 m long from the main rock body, which slipped down towards the Raunthi Gadera valley floor, causing massive devastation in the areas such as Raini, Tapovan, and Vishnuprayag. This event was not expected and was the first event in history when a flash flood occurred in winter. In this study, we tried to answer two major questions which are not been explained so far that are related to this disaster. These questions are (i) why did this event occur in winters? (ii) where did so much debris and water come from?. This study clearly answers these questions based on field observationsKeywords
Flash Flood, Himalaya, Nanda Devi, Raunthi Gadera, Rishiganga.References
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