Erosion in High Tidal Mudflats

Extensive Erosion of Mudflats Changes Shoreline in Gulf Of Khambhat

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Tidal mudflats of Gulf of Khambhat on west coast constitute an important ecosystem on India’s coastline. Scientists have now found that these mudflats are experiencing severe erosion which is threatening the vital habitat.

Scientists from the Ahmedabad-based Space Applications Centre (SAC) of Indian Space Research Organisation (ISRO) have reported extensive erosion of mudflats by studying sequential satellite images. Scientists analyzed temporal satellite images to understand the hydrodynamics and coastal processes along the northern part of the Gulf of Khambhat.

 

Erosion in High Tidal Mudflats
Erosion in High Tidal Mudflats

The Gulf of Khambhat is a tidal regime in the Arabian Sea formed at the mouth of major rivers Tapti, Narmada, Mahi, Sabarmati that form estuaries along the west coast.

The researchers found that a total of about 28.66 sq km area of high tidal mudflats has got eroded within a span of just three and a half years – from March 2014 to September 2017. The erosion rate was observed to be very high at 3.5 to 4 km per year, according to results of the study recently published in journal Current Science.

Satellite Images before and after erosion
Satellite Images before and after erosion

The erosion is higher in winter and pre-monsoon seasons than during the summer monsoon. It appears to be because of the high input of fresh water during the summer monsoon, which prevents the strengthening of current velocity during high tide. Although high tidal mudflats are rarely flooded even under high tide conditions, extensively high erosion has been observed along the 20 km long stretch and about 3 km inside. The high rate of erosion has changed the shoreline.

“The high erosion is due to the meandering tidal channels that connect Mahi river to the Gulf. The strong tidal current along the outer boundary of meandering river carved the channel and tidal channel migrate towards the land side” explained Dr. Ratheesh Ramakrishnan, senior scientist, and research team leader, while speaking to India Science Wire.

Hiren Bhatti in the field work at Gulf of Khambhat
Hiren Bhatti in the field work at Gulf of Khambhat

Tidal flats or Mudflats are deposits of mud, silt, and clay made by tides or rivers along a coast. They are found in sheltered areas such as bays, bayous, lagoons and estuaries and range from soft muds to firm sands.  Mudflats can be categorized into three distinct zones – sub-tidal (shallow underwater deposits) zone, middle intertidal zone, and upper supra-tidal zone or high tidal mudflats.

The high tidal mudflats are the least inundated and are submerged only at high tide. They are usually covered with vegetation and are characterized by fine-grained deposits consisting of clay and fine silt.

Noting that the Gulf of Khambhat is a hotspot for major development activities, researchers hoped the study will help to ensure that the mudflats are saved before they are destroyed totally.

The research team included Hiren Bhatti, Ratheesh Ramakrishnan, A. K. Sharma and A. S. Rajawat. (India Science Wire)

Dr. Ravi Mishra

Journal Article

Incessant erosion of high tidal mudflats in the northern Gulf of Khambhat

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Erosion in High Tidal Mudflats
Erosion in High Tidal Mudflats

The Gulf of Khambhat is a tidal regime in the Arabian Sea formed at the mouth of major rivers Tapti, Narmada, Mahi, Sabarmati that form estuaries along the west coast.

The researchers found that a total of about 28.66 sq km area of high tidal mudflats has got eroded within a span of just three and a half years – from March 2014 to September 2017. The erosion rate was observed to be very high at 3.5 to 4 km per year, according to results of the study recently published in journal Current Science.

Satellite Images before and after erosion
Satellite Images before and after erosion

The erosion is higher in winter and pre-monsoon seasons than during the summer monsoon. It appears to be because of the high input of fresh water during the summer monsoon, which prevents the strengthening of current velocity during high tide. Although high tidal mudflats are rarely flooded even under high tide conditions, extensively high erosion has been observed along the 20 km long stretch and about 3 km inside. The high rate of erosion has changed the shoreline.

“The high erosion is due to the meandering tidal channels that connect Mahi river to the Gulf. The strong tidal current along the outer boundary of meandering river carved the channel and tidal channel migrate towards the land side” explained Dr. Ratheesh Ramakrishnan, senior scientist, and research team leader, while speaking to India Science Wire.

Hiren Bhatti in the field work at Gulf of Khambhat
Hiren Bhatti in the field work at Gulf of Khambhat

Tidal flats or Mudflats are deposits of mud, silt, and clay made by tides or rivers along a coast. They are found in sheltered areas such as bays, bayous, lagoons and estuaries and range from soft muds to firm sands.  Mudflats can be categorized into three distinct zones – sub-tidal (shallow underwater deposits) zone, middle intertidal zone, and upper supra-tidal zone or high tidal mudflats.

The high tidal mudflats are the least inundated and are submerged only at high tide. They are usually covered with vegetation and are characterized by fine-grained deposits consisting of clay and fine silt.

Noting that the Gulf of Khambhat is a hotspot for major development activities, researchers hoped the study will help to ensure that the mudflats are saved before they are destroyed totally.

The research team included Hiren Bhatti, Ratheesh Ramakrishnan, A. K. Sharma and A. S. Rajawat. (India Science Wire)

Dr. Ravi Mishra

Journal Article

Incessant erosion of high tidal mudflats in the northern Gulf of Khambhat

If you liked this article, then please subscribe to our YouTube Channel for the latest Science and Tech news. You can also find us on Twitter and Facebook.

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