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Evaluation of 3D structural changes in general atmospheric and monsoon circulations during Kedarnath disaster (India), 16–17 June 2013

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Abstract

Intense rains on 16–17 June 2013 over Mandakini River catchment caused Kedarnath disaster in Uttarakhand State (India). Normal and departure-from-normal 3D global atmospheric thermal structure and general and monsoon circulations during the event have been compared using equatorially/globally- conditioned surface and upper air parameters (1000–100 hPa) (period: 1979–2013). Briefly, normal monsoon structure is: 1000‒850 hPa layer- cross-equatorial flows over Indian Ocean and Eurasian westerlies confluence over Indian domain, the two flows further confluence downstream with Pacific easterlies and then the accumulated airmasses blow northeastward; 700‒500 hPa layer- Eurasian westerlies after sweeping entire Indian subcontinent make exit northeastward; and 400‒100 hPa layer- upper tropospheric anticyclone well-developed over subtropical Asia and outflows are spread all around. On 16–17 June 2013, two upper tropospheric anticyclonic cells occurred, one over Tibet-China and another Mediterranean-Middle East. Troposphere (1000–250 hPa) was significantly warmer-and-thicker over Tibet-China followed by Mediterranean-Middle East while cooler-and-thinner over central Asia-India sector. Departures in downward slopes of tropospheric temperature and thickness from Tibet-China outward were significantly steeper. A huge trough evolved over Indo-Pacific region from an interaction between Eurasian westerlies and Indo-Pacific easterlies, and outflows from the trough made forced exit through western Himalaya which modulated north mid-high latitudes westerlies into a single wave structure. Combined five factors produced disastrous rains over Kedarnath: cool-low and warm-low regime contrast; squeezing of deep warm-moist flows; orographic lifting; and pumping and suction effects. Forced warm-moist outflows from Indo-Pacific region caused warmer-thicker troposphere over eastern Russia-North America. Lesser outflows from Tibet-China anticyclone were directed southward, consequently troposphere was cooler-thinner over southern mid-high latitudes.

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Abbreviations

AIP:

Asia-Indo-Pacific

CA-IND:

Central Asia – India

CH:

Cool-high

CL:

Cool-low

EC-mslp:

Equatorially Conditioned mean sea level pressure

EC-PW:

Equatorially Conditioned Precipitable Water

EC-Tlevel :

Equatorially Conditioned Temperature at particular level

EC-TTROP :

Equatorially Conditioned Tropospheric temperature

EC-Zlevel :

Equatorially Conditioned geopotential height at particular level

EC-ZTROP :

Equatorially Conditioned Tropospheric Thickness

EMV:

Equatorial Mean Value

EREs:

Extreme Rain Events

GC-W:

Globally Conditioned Wind Speed

GMV:

Global Mean Value

GWRs:

Global Weather Regimes

LOSSI:

Location, orientation, shape, size and intensity

MME:

Mediterranean – Middle East

NH:

Northern Hemisphere

NPL:

North Polar

NSBT:

North Subtropic

SH:

Southern Hemisphere

SPL:

South Polar

SSBT:

South Subtropic

TBT-CHN:

Tibet-China

WL:

Warm-low

WH:

Warm-high

References

  • Ashrit R (2010) A report on investigating the Leh cloudburst. NCMRWF report No. NMRF/RR/2010, 18pp

  • Bohlinger P, Sorteberg A, Sodemann H (2017) Synoptic conditions and moisture sources actuating extreme precipitation in Nepal. J Geophys Res 122(12):653–671

    Google Scholar 

  • Bohlinger P, Sorteberg A, Liu C, Rasmussen R, Sodemann H, Ogawa F (2019) Multiscale characteristics of an extreme precipitation event over Nepal. Q J R M S 145:179–196. https://doi.org/10.1002/qj.3418

    Article  Google Scholar 

  • Chaudhari C, Tripathi S, Srivastava R, Misra A (2015) Observation- and numerical -analysis-based dynamics of the Uttarkashi cloudburst. Ann Geophys 33:671–686

    Article  Google Scholar 

  • Chevuturi A, Dimari AP (2016) Investigation of Uttarakhand (India) disaster-2013 using weather research and forecasting model. Nat Hazards 82(3):1703–1726

    Article  Google Scholar 

  • Chevuturi A, Dimari AP, Das S, Kumar A, Niyogi D (2015) Numerical simulation of an intense precipitation event over Rudraprayag in the central Himalyas during 13–14 September 2012. J Earth Syst Sci 124(7):1545–1561

    Article  Google Scholar 

  • Cho C, Li R, Wang S, Yoon JH, Gillies, RR (2015) Anthropogenic footprint of climate change in the June 2013 northern India flood. Plants, Soils, and Climate Faculty Publications. Paper 735, 26pp

  • Dobhal DP, Gupta AK, Mehta M, Khandelwal DD (2013) Kedarnath disaster: facts and plausible causes. Curr Sci 105(2):171–174

    Google Scholar 

  • Dube A, Ashrit R, Ashish A, Sharma K, Iyengar GR, Rajagopal EN, Basu S (2014) Forecasting the heavy rainfall during Himalayan flooding-June 2013. Weather Clim Extremes 4:22–34

    Article  Google Scholar 

  • Dubey CS, Shukla DP, Ningreichon AS, Usham AL (2013) Orographic control of the Kedarnath disaster. Curr Sci 105(11):1474–1476

    Google Scholar 

  • Hong CC, Hsu HH, Lin NH, Chiu H (2011) Roles of European blocking and tropical-extratropical interaction in the 2010 Pakistan flooding. Geophy Res Lett 38:L13806. https://doi.org/10.1029/2011GL047583

    Article  Google Scholar 

  • Houze RA, Rasmussen KL, Medina S, Brodzik SR, Romatschke U (2011) Anomalous atmospheric events leading to the summer 2010 floods in Pakistan. Bull Am Meteor Soc 92:291–298

    Article  Google Scholar 

  • Houze RA, McMurdie LA, Rasmuseen KL, Kumar A, Chaplin MM (2017) Multiscale aspects of the storm producing the June 2013 flooding in Uttarakhand, India. Mon Wea Rev 145(11):4447–4466. https://doi.org/10.1175/MWR-D-17-0004.1

    Article  Google Scholar 

  • Joseph S, Sahai AK, Sharmila S, Abhilash S, Borah N, Chattopadhyay R, Pillai PA, Rajeevan M, Kumar A (2015) North Indian heavy rainfall event during June 2013: diagnostics and extended range prediction. Clim Dyn 44:2049–2065

    Article  Google Scholar 

  • Kotal SD, Roy SS, Bhowmik SKR (2014) Catastrophic heavy rainfall episode over Uttarakhand during 16–18 June 2013—observational aspects. Curr Sci 107(2):234–245

    Google Scholar 

  • Krishnamurti TN, Kumar V, Simon A, Thomas A, Bhardwaj A, Das S, Sen Roy S, Roy Bhowmik RK (2017) March of buoyancy elements during extreme rainfall over India. Clim Dyn 48:1931–1951

    Article  Google Scholar 

  • Kumar A, Houze RA, Rasmussen KL (2014) Simulation of a flash flooding storm at the steep edge of the Himalyas. J Hydrometeorol 15:212–228

    Article  Google Scholar 

  • Lau W, Kim KM (2012) The 2010 Pakistan and Russian heat wave: teleconnection of hydro -meteorological extremes. J Hydrometerol 13:392–403

    Article  Google Scholar 

  • Martha TR, Roy P, Govindraj KB, Kumar V, Diwakar PG, Dhadwal VK (2015) Landslides triggered by the June 2013 extreme rainfall event in parts of Uttarakhand state, India. Landslides 12:135–146

    Article  Google Scholar 

  • Mishra A, Srinivasan J (2013) Did a cloud burst occur in Kedarnath during 16 and 17 June 2013? Curr Sci 105(10):1351–1352

    Google Scholar 

  • NATMO (1986) National Atlas of India Physiographic Regions of India. Third edition, Plate 41, Prepared under the Direction of G.K. Dutt, Director, NATMO (the National Atlas & Thematic Mapping Organization), Kolkata, India

  • Parida BR, Behera SN, Bakimchandra O, Pandey AC, Singh N (2017) Evaluation of satellite-derived rainfall estimates for an extreme rainfall event over Uttarakhand, Western Himalayas. Hydrology 22(4):1–18. https://doi.org/10.3390/hydrology4020022

    Article  Google Scholar 

  • Priya P, Krishnan R, Mujumdar M, Houze RA Jr (2017) Changing monsoon and midlatitude circulation interactions over the Western Himalayas and possible links to occurrences of extreme precipitation. Clim Dyn 49:2351–2364

    Article  Google Scholar 

  • Rajeevan M, Bhate J (2008) A high resolution daily gridded rainfall Data Set (1971–2005) for Mesoscale Meteorological Studies. National Climate Center, India meteorological Department, Research Report No.9, 14pp

  • Ranade A, Singh N (2019) Equatorially/Globally conditioned meteorological analysis of heaviest rains over India during 23–28 July 2005. Meteorol Atmos Phys 131(4):919–944. https://doi.org/10.1007/s00703-018-0613-6

    Article  Google Scholar 

  • Ranalkar MR, Chaudlhari HS, Hazra A, Sawaisarje GK, Pokhrel S (2016) Dynamical features of incessant heavy rainfall event of June 2013 over Uttarakhand, India. Nat Hazards 80:1579–1601

    Article  Google Scholar 

  • Rasmussen KL, Houze RA (2012) A flash-flooding storm at the steep edge of high terrain: disaster in the Himalayas. Bull Am Met Soc 93:1713–1724

    Article  Google Scholar 

  • Rasmussen KL, Hill AJ, Toma VE, Zuluaga MD, Webster PJ, Houze RA (2015) Multiscale analysis of three consecutive years of anomalous flooding in Pakistan. Quart J R Met Soc 141:1259–1276

    Article  Google Scholar 

  • Ray C, Chattoraj PK, Bisht SL, MPS et al (2016) Kedarnath disaster 2013: causes and consequences using remote sensing inputs. Nat Hazards 81:227–243

    Article  Google Scholar 

  • Saha S et al (2010) The NCEP climate forecast system reanalysis. Bull Am Meteorol Soc 91(8):1015–1057. https://doi.org/10.1175/2010BAMS3001.1

    Article  Google Scholar 

  • Saha S et al (2014) The NCEP climate forecast system version 2. J Clim 27:2185–2208. https://doi.org/10.1175/JCLI-D-12-00823.1

    Article  Google Scholar 

  • Sati VP (2013) Extreme weather-related disasters: a case study of two flash floods hit areas of Badrinath and Kedarnath valleys, Uttarakhand Himalaya, India. J Earth Sci Engg 3:562–568

    Google Scholar 

  • Shekhar MS, Pattanayak S, Mohanty UC, Paul S, Sravana Kumar SM (2015) A study on the heavy rainfall event around Kedarnath area (Uttarakhand) on 16 June 2013. J Earth Syst Sci 124(7):1531–1544

    Article  Google Scholar 

  • Singh D, Horton DE, Tsiang T, Haugen M, Ashfaq M, Mei R, Rastogi D, Johnson NC, Charland A, Rajaratnam B, Diffenbaugh NS (2014) Severe precipitation in Northern India in June 2013: causes, historical context, and changes in probability. Bull Am Meteorol Soc 95(9):558–561

    Google Scholar 

  • Srinivasan J (2013) Predicting and managing extreme rainfall. Curr Sci 105:7–8

    Google Scholar 

  • Thayyen R, Dimri AP, Kumar P, Agnihotri G (2013) Study of cloudburst and flash floods around Leh, India during August 4–6, 2010. Natur Hazards 65(3):2175–2204

    Article  Google Scholar 

  • Vellore RK, Kaplan ML, Krishnan R, Lewis JM, Sabade S, Deshpande N, Singh BB, Madhura RK, Rama Rao MVS (2016) Monsoon-extratropical circulation interactions in Himalayan extreme rainfall. Clim Dyn 46:3517–3546

    Article  Google Scholar 

  • Vellore RK, Bisht JS, Krishnan R, Uppara U, Capua GD, Coumou D (2019) Sub-synoptic circulation variability in the Himalayan extreme precipitation event during June 2013. Meteorol Atmos Phys. https://doi.org/10.1007/s00703-019-00713-5

    Article  Google Scholar 

  • Webster PJ, Toma VE, Kim HM (2011) Were the 2010 Pakistan floods predictable? Geophys Res Lett 38:L04806

    Article  Google Scholar 

Download references

Acknowledgements

First author is extremely gratefully to Director, National Institute of Hydrology, Roorkee for necessary facilities to pursue the study, and to the Department of Science and Technology (DST), Govt. of India for sponsoring this research project.

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Authors and Affiliations

  1. Surface Water Hydrology Division, National Institute of Hydrology, Roorkee, Uttarakhand, 247667, India

    Ranade Ashwini

  2. Indian Institute of Tropical Meteorology, Dr. Homi Bhabha Road, Pashan, Pune, Maharashtra, 411008, India

    Singh Nityanand

  3. 9, Pashan Villa, Pashan, Pune, Maharashtra, 411021, India

    Singh Nityanand

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  1. Ranade Ashwini
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Correspondence to Ranade Ashwini.

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Ashwini, R., Nityanand, S. Evaluation of 3D structural changes in general atmospheric and monsoon circulations during Kedarnath disaster (India), 16–17 June 2013. Meteorol Atmos Phys 133, 857–878 (2021). https://doi.org/10.1007/s00703-021-00780-7

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