NISAR SATELLITE AND SEISMIC ZONES - GEOGRAPHY

News: NISAR satellite to map Himalayas’ seismic zones

 

What's in the news?

       A forthcoming satellite, NISAR will map the most earthquake-prone regions in the Himalayas with unprecedented regularity.

 

About the mapping:

       The data this will generate can potentially give advance warning of land subsidence, as recently observed in Joshimath, Uttarakhand, as well point to places that are at greatest risk from earthquakes.

       The NISAR satellite will use two frequency bands: the L-band and S-band to image the seismically active Himalayan region that will, every 12 days, create a “deformation map”.

       The geoscience community can use this to determine how strain is building up in various parts of the Himalayas.

       These two frequency bands will together provide high-resolution, all-weather data from the satellite that is expected to follow a sun-synchronous orbit and will be launched in January 2024.

 

About the Himalayan strain:

       Strain refers to the deformation that occurs in rocks when it is under pressure from other rocks, usually due to movements of continental plates that are sliding, colliding, or subducting against each other.

       The Indian Plate, for instance, collided into the Eurasian plate forming the Himalayas and continues to incrementally push it upwards.

 

Strain map:

       Scientists from the Geological Survey of India in 2021 published a “strain map” of the Himalayas based on data from 1,252 GPS stations along the Himalayas.

       It identified regions that had the greatest odds of generating earthquakes of magnitude above 8 and their extent.

       With a frequency of 12 days and the ability to be able to provide images even under cloudy conditions, NISAR would be a valuable tool to study deformation patterns, such as in Joshimath.

       Based on the intensity of past earthquakes, the knowledge of the speed at which plates move and the locations at which plates interact (called faults) can help geologists and seismologists map out regions that are most vulnerable to earthquakes and estimate how far the resultant tremors can spread.

       Ground-based observatories can pick up underground waves that result from an earthquake and provide early warning.

       Uttarakhand case: Land subsidence or the loosening of the sub-surface had caused several parts of Uttarakhand to “sink” and this caused water to seep via cracks and crevices into houses.

       In 2021, a large landslide of rock and ice triggered a flash flood in Chamoli, Uttarakhand that claimed close to 200 lives and destroyed two hydropower projects. It was satellite imagery that helped scientists decipher the cause of the flash floods.

 

About NISAR mission:

Developed by: National Aeronautics and Space Administration (NASA) and the Indian Space Research Organisation (ISRO).

 

Launch:

       It is expected to be launched in January 2024 from Satish Dhawan Space Centre into a near-polar orbit.

 

Features:

       The satellite will operate for a minimum of three years.

       It is a Low Earth Orbit (LEO) observatory.

       NISAR will map the entire globe in 12 days.

       The 2,800kilogram satellite is a dual-frequency imaging radar satellite.

       While NASA has provided the L-band radar, GPS, a high-capacity solid-state recorder to store data, and a payload data subsystem, ISRO has provided the S-band radar, the GSLV launch system and spacecraft.

       Another important component of the satellite is its large 39-foot stationary antenna reflector.

       The reflector will be used to focus “the radar signals emitted and received by the upward-facing feed on the instrument structure.

 

Objectives:

       Synthetic Aperture Radar mission is to determine Earth change in three disciplines:

       Ecosystems (vegetation and the carbon cycle).

       Deformation (solid Earth studies).

       Cryosphere sciences (primarily as related to climatic drivers and effects on sea level).

 

Seismic zone mapping:

       Over 59 % of India’s land area is under threat of moderate to severe earthquakes.

       The Bureau of Indian Standards, based on the past seismic history, divided the country into four seismic zones, viz. Zone II, III, IV and V.

       The zones are divided on the basis of Modified Mercalli (MM) intensity, which measures the impact of earthquakes.

 

Types of seismic zones:

1. Zone II:

       This is seismically the least active region. It covers parts of India that are not included in Zone III, IV and V.

2. Zone III:

       Comprises Kerala, Goa, Lakshadweep islands, remaining parts of Uttar Pradesh, Gujarat and West Bengal, Parts of Punjab, Rajasthan, Madhya Pradesh, Bihar, Jharkhand, Chhattisgarh, Maharashtra, Orissa, Andhra Pradesh, Tamil Nadu and Karnataka.

3. Zone IV:

       It covers parts of Jammu and Kashmir and Himachal Pradesh, National Capital Territory (NCT) of Delhi, Sikkim, Northern parts of Uttar Pradesh, Bihar and West Bengal, parts of Gujarat and small portions of Maharashtra near the west coast and Rajasthan.

4. Zone V:

       This is seismically the most active region. Parts of the Himalayan boundary in North and Northeast India fall in this zone.

       The Kutch area in the West also falls here. Remaining parts of Jammu and Kashmir, Himachal Pradesh, Uttaranchal, part of North Bihar and Andaman and the Nicobar Islands are included.