Karachi tides during the 1945 Makran tsunami

Abstract This paper extends and detides a Karachi tide-gauge record as an observational basis for assessing Indian Ocean tsunami risk. The extended marigram encompasses the time of the great 1945 Makran earthquake of early November 28, local time, and of the ensuing tsunami, which continued into Nov...

Full description

Bibliographic Details
Main Authors: Loyce M. Adams, Brian F. Atwater, Haider Hasan
Format: Article
Language:English
Published: SpringerOpen 2018-09-01
Series:Geoscience Letters
Subjects:
Online Access:http://link.springer.com/article/10.1186/s40562-018-0121-z
id doaj-0ea3dad5b6aa4af2b9d2b1f67e46c300
record_format Article
spelling doaj-0ea3dad5b6aa4af2b9d2b1f67e46c3002020-11-25T02:29:18ZengSpringerOpenGeoscience Letters2196-40922018-09-015111310.1186/s40562-018-0121-zKarachi tides during the 1945 Makran tsunamiLoyce M. Adams0Brian F. Atwater1Haider Hasan2Department of Applied Mathematics, University of WashingtonU.S. Geological Survey at University of WashingtonDepartment of Civil Engineering, NED University of Engineering and TechnologyAbstract This paper extends and detides a Karachi tide-gauge record as an observational basis for assessing Indian Ocean tsunami risk. The extended marigram encompasses the time of the great 1945 Makran earthquake of early November 28, local time, and of the ensuing tsunami, which continued into November 29. The marigram was published previously as a 9-h excerpt that begins 1 h after the earthquake. The full marigram presented here covers most of 17 days from November 15 to December 1. Gaps include a tsunami-induced outage that may help explain why the highest water level gauged is 1 m below the maximum water level reported nearby. The detiding method computes a reference tidal curve that disregards all observations from November 28 and 29. For those 2 days, the reference tide is guided by Admiralty tide tables and, secondarily, by high waters and low waters gauged before and after. As in previous estimates, the detided tsunami crests about 0.5 m above ambient tide, but now with the possibility that the gauge failed to record a higher wave. Anomalies described for the first time include an early one that likely resulted from a recognized problem with the Karachi tide station, but which might instead represent an earthquake precursor.http://link.springer.com/article/10.1186/s40562-018-0121-zTsunamiTide gaugeMakranKarachi
collection DOAJ
language English
format Article
sources DOAJ
author Loyce M. Adams
Brian F. Atwater
Haider Hasan
spellingShingle Loyce M. Adams
Brian F. Atwater
Haider Hasan
Karachi tides during the 1945 Makran tsunami
Geoscience Letters
Tsunami
Tide gauge
Makran
Karachi
author_facet Loyce M. Adams
Brian F. Atwater
Haider Hasan
author_sort Loyce M. Adams
title Karachi tides during the 1945 Makran tsunami
title_short Karachi tides during the 1945 Makran tsunami
title_full Karachi tides during the 1945 Makran tsunami
title_fullStr Karachi tides during the 1945 Makran tsunami
title_full_unstemmed Karachi tides during the 1945 Makran tsunami
title_sort karachi tides during the 1945 makran tsunami
publisher SpringerOpen
series Geoscience Letters
issn 2196-4092
publishDate 2018-09-01
description Abstract This paper extends and detides a Karachi tide-gauge record as an observational basis for assessing Indian Ocean tsunami risk. The extended marigram encompasses the time of the great 1945 Makran earthquake of early November 28, local time, and of the ensuing tsunami, which continued into November 29. The marigram was published previously as a 9-h excerpt that begins 1 h after the earthquake. The full marigram presented here covers most of 17 days from November 15 to December 1. Gaps include a tsunami-induced outage that may help explain why the highest water level gauged is 1 m below the maximum water level reported nearby. The detiding method computes a reference tidal curve that disregards all observations from November 28 and 29. For those 2 days, the reference tide is guided by Admiralty tide tables and, secondarily, by high waters and low waters gauged before and after. As in previous estimates, the detided tsunami crests about 0.5 m above ambient tide, but now with the possibility that the gauge failed to record a higher wave. Anomalies described for the first time include an early one that likely resulted from a recognized problem with the Karachi tide station, but which might instead represent an earthquake precursor.
topic Tsunami
Tide gauge
Makran
Karachi
url http://link.springer.com/article/10.1186/s40562-018-0121-z
work_keys_str_mv AT loycemadams karachitidesduringthe1945makrantsunami
AT brianfatwater karachitidesduringthe1945makrantsunami
AT haiderhasan karachitidesduringthe1945makrantsunami
_version_ 1724833853282975744