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European Journal of Applied Sciences – Vol.10, No.5

Publication Date: October 25, 2022

DOI:10.14738/aivp.105.12641.

Faheed, J. K. P., Yusuf, A., Manjusree, P., & Ansari, Z. R. (2022). Monitoring of Flood Dynamics Using Multi Temporal Satellite Data:

A Case Study of Kerala Floods 2018. European Journal of Applied Sciences, 10(5).443-480.

Services for Science and Education – United Kingdom

Monitoring of Flood Dynamics Using Multi Temporal Satellite

Data: A Case Study of Kerala Floods 2018

Faheed Jasin K. P.

Interdisciplinary Department of Remote Sensing &

GIS Applications, A.M.U., Aligarh

Alia Yusuf

Geology Section, Women’s College

Aligarh Muslim University, Aligarh, U.P., INDIA

P. Manjusree

National Remote Sensing Centre, Deptt. of ISRO

Govt of India, Balanagar, Hyderabad

Ziaur Rehman Ansari

Interdisciplinary Department of Remote Sensing &

GIS Applications, A.M.U., Aligarh

ABSTRACT

India is one of the worst flood affected country in South East Asia and accounts for

one fifth of global death count due to floods. It causes heavy losses to property,

infrastructure, agriculture, land and overburdens the country's budget and

resources. Around 40 million hectares of land in the country are subjected to

floods according to National Flood Commission, and an average of 18.6 million

hectares of land is affected annually. During 2018, Kerala was hit by two flood

events in July and August. In August, 2018, Kerala experienced the worst ever

floods in its history since 1924. The torrential rains triggered several landslides

and forced the release of excess water from 37 dams across the state, aggravating

the flood impact. The devastating floods and landslides caused extensive damage

to houses, roads, railways, bridges, power supplies, communications networks,

and other infrastructure. Satellite Remote Sensing has made substantial

contribution in flood monitoring and damage assessment. The unique capabilities

of satellites to provide comprehensive, synoptic and multi-temporal coverage of

very large areas at regular interval and with quick turnaround time have been

very valuable in monitoring and managing flood dynamics. The microwave region

of the EM spectrum has a greater potential in identification of flooded areas

because of almost all weather capability. In this study, multi-temporal microwave

SAR data from RADARSAT and SENTINEL-1 satellites was used to map the flood

affected areas in Kerala and to capture the dynamics of the spatial flood extent.

The analysis showed maximum flood inundation in the second flood event in

August. A steady recession of flood was observed in the July flood event. The peak

flooding was observed on 18th August 2018. There is a rapid progression of flood

from August 11th to August 18th 2018 after which, a slight recession was observed

from August 18th to 21st ,2018. The flood could be seen slightly progressing in the

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European Journal of Applied Sciences (EJAS) Vol.10, Issue 5, October-2022

Services for Science and Education – United Kingdom

next interval of August 21stto 24th ,2018 after which, again an overall recession in

the spatial flood could be observed by 27th August 2018. Kottayam,

Pathanamthitta and Alappuzha were some of the worst flood affected districts. The

maximum flood affected district is observed to be Alappuzha with a maximum

flood inundated area of 27691hectares on 18 August 2018. In the district of

Alappuzha a steady progression in the flood is observed after 21 August. Whereas

in the other two districts namely Kottayam, Pathanamthitta the flood is found to

be receeding after August 24, 2018.This study demonstrated the potential of

multi-temporal satellite imageries for capturing the flood dynamics in a spatial

domain. The progression and recession maps can be used for relief management

by the disaster managers on the ground.

Keywords: Synthetic Aperture Radar, RADARSAT, SENTINEL-1, Flood Dynamics, Flood

Analysis and Microwave Remote Sensing

INTRODUCTION

With the long term change in weather pattern, incidences of extreme heat and humidity are

rising which manifests itself as global increase in precipitation events and subsequent

riverine and flash flood is the manifestation of climate change [1]. According to Federal

Emergency Management Agency (FEMA) Flood is defined as a general or temporary condition

of partial or complete inundation of normally dry land areas from the overflow of inland or

tidal waters and unusual rapid accumulation or run off of surface waters from any source.

These climate change events occur in India as well on frequent basis. Severe floods occur

almost every year in one or the other part of the country causing tremendous loss of life, large

scale damage to property, infrastructure, agriculture, land and overburdens the countries

budget and resources. Floods mostly occur in the country during the south west monsoon

period spread from June to September, though cyclonic storms are common during October to

December. India is the worst flood affected country in the world after Bangladesh and

accounts for one fifth of global death count due to floods. Around 40 million hectares of land

in the country are subjected to floods according to National Flood Commission and an average

of 18.6 million hectares of land is affected annually. To avoid such catastrophic loss of life and

property it is necessary to map the events of flood in entire country so that better planning for

disaster management can be done.

KERALA FLOODS 2018

A catastrophic flood event which devastated the southern state of Kerala, India took place in

2018 due to unprecedented heavy rainfall from 1 June –18 August 2018. The normal

cumulative rainfall during monsoons in Kerala from June till end of August is around 1795.4

mm, but during 2018 monsoon it got an actual cumulative rainfall more than 2428.9 mm was

reported by Indian Meteorological Department (IMD) and Central Water Commission

(CWC). All of major 35 odd reservoirs storage was close to the full reservoir level (FRL) and

had no buffer storage to accommodate the heavy inflows from 10th August. The continued

exceptional heavy rainfall in August (with 170% above normal) in the catchment areas had

compelled the authorities to resort to heavy releases downstream into the rivers. Such a

scenario that continued for almost a week has caused overflowing of all river banks leading to

widespread flooding almost all over the state. During the week of 9th to 15thAugust the rainfall

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Faheed, J. K. P., Yusuf, A., Manjusree, P., & Ansari, Z. R. (2022). Monitoring of Flood Dynamics Using Multi Temporal Satellite Data: A Case Study

of Kerala Floods 2018. European Journal of Applied Sciences, 10(5).443-480.

URL: http://dx.doi.org/10.14738/aivp.105.12641

was severe and Kerala received 255% extra rainfall (Fig.1). Idukki district in which major

dams are situated received 679mm of rain just during that week, the normal during that

period is only 126 mm, which is 438% extra rain. That leads to the opening of Idukki dam

after 26 years. Wayanad received 536.8mm rainfall which is 299% extra for that hilly district,

the normal rainfall for Wayanad is only 134mm [2]. This incessant rainfall triggered

landslides and snapped road links between Wayanad and rest of Kerala. This catastrophic

disaster had created loss of life and property in a dimension unexpected. About 400 people

were reported dead in the state and over 1 million people moved to relief and rescue camps.

According to the Kerala government, one-sixth of the total population of Kerala had been

directly affected by the floods and related incidents, 13 out of 14 districts of Kerala were

affected by the event.

The Indian government had declared it a Level 3 Calamity or "calamity of a severe nature”.

Thirty-five out of the fifty-four dams within the state were opened, for the first time in history.

All five overflow gates of the Idukki Dam were opened at the same time and for the first time

in 26 years 5 gates of the Malampuzha dam of Palakkad were opened. Heavy rains

in Wayanad and Idukki have caused severe landslides and have left the hilly districts isolated.

Such catastrophic events require immediate attention and hence should be mapped to

understand the dynamics of the river. Earth observation data is very useful and essential tool

for flood monitoring[3], risk assessment [4,5], modelling, prediction and validation for

weather forecasting and rainfall-runoff models. These technologies have been the object of

substantial interest for all countries and bodies concerned with space and in exacting

emergency services and disaster management[6]. Remote Sensing along with has proven to

be very effectively for quick assessment of severity and impact caused by natural disasters.

Observed Rainfall as on 11-Aug Observed Rainfall as on 12-Aug Observed Rainfall as on 13-Aug