dc.description.abstract |
Part of North-Western Himalaya, Which typically comprised of, Jammu and Kashmir,
Laddakh, Himachal Pradesh, and Uttarakhand, particularly Uttarakhand, has been
identified by several eminent seismologists as a gap area where large size
earthquake( greater than magnitude 7) is expected. The region has
witnessed two earthquakes having a magnitude greater than 6 in the last 25
years ( 28th March 1999 Chamoli earthquake and 20th October 1991 Uttarkashi
earthquake ), both having an epicenter in the Garhwal region of Uttarakhand. Several
studies have shown that a future large earthquake in Central Himalayas can generate
severe ground motion in the National capital region of Delhi, which is about 300 km from
this expected source. Several densely populated cities and villages having a total
population of several million are located between Delhi and Uttarakhand. These
towns/cities will be severely affected by a large earthquake having an epicenter in this
region. Using advancements in communication technology and real-time seismology, a
project to have an earthquake early warning system for Northern India is under progress
at the Indian Institute of Technology, Roorkee. In this project, a dense network of 84
accelerometers has been installed, covering an area of about 100 km x 40 km in the
Garhwal region. This network has an intermediate station to station distance of less than
10km, and all the sensors are streaming data, which is being processed in real-time at the
central server stationed at Roorkee. The cost of the sensor becomes one of the most
important parameters on which the viability of an Earthquake Early Warning (EEW)
system depends since a dense network of the sensor is required for an effective EEW
system. Thus in this study, a detailed analysis is also performed to find out the optimum
dynamic range of sensor that is required so that the most relevant information, EEW
parameter, and strong motion parameters could be retrieved from the obtained ground
motion data. In the study, it is observed that for all relevant EEW parameters, a sensor
with ADC with the 16-Bit resolution is quite sufficient, and most of the required
information could be retrieved from such data. This thesis describes details of the
network, sensors, present status of development, performance of instrumentation during
recent events and processing details. The thesis also provides details of the theoretical
and numerical analysis done for the ADC dynamic range varying from 24-Bit to 10-Bit
and its impact on the most relevant EEW parameter and strong motion parameters. A new approach for P-phase picking has also been developed in this study. The parameter
used is ‘Damage Intensity’ which has been widely used in Japan for intensity estimation
for UrEDAS. One of the problems faced during the testing of the EEW system was to
eliminate far-field earthquakes. By far-field events are those events that have their
epicenter at a large distance from the networked region. During testing, one such event
from the Hindukush region was picked by the software. Thus it was a concern that such
events should not be picked or, if picked, should be ignored by the EEW system. Using
this approach, it was found that far-field earthquakes could be eliminated and were not
picked if this approach is used. |
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