Comparison of sea surface heights observed by TOPEX altimeter with sea level data at Chichijima

1996 ◽  
Vol 52 (3) ◽  
pp. 259-273 ◽  
Author(s):  
Naoto Ebuchi ◽  
Kimio Hanawa
Keyword(s):  
Sea Level ◽  
Sea Surface ◽  
Level Data ◽  
Sea Surface Heights

scholarly journals SPATIO-TEMPORAL CHARACTERISTICS OF SEA LEVEL ANOMALY IN THE INDONESIAN WATER

GEOMATIKA ◽  
2019 ◽  
Vol 25 (2) ◽  
pp. 103
Author(s):  
Dina Anggreni Sarsito ◽  
Dudy Darmawan Wijaya ◽  
Nur Fajar Trihantoro ◽  
Muhammad Syahrullah Fathulhuda ◽  
Dhota Pradipta
Keyword(s):  
Sea Level ◽  
Geographical Location ◽  
Sea Surface Height ◽  
Sea Surface ◽  
Sea Level Anomaly ◽  
Level Data ◽  
Mean Sea Surface ◽  
Spatio Temporal ◽  
East Asia Region ◽  
The Impact

<p>Indonesia is an archipelago state lies between Indian and Pacific Oceans at the South East Asia region. Its unique geomorphological and geographical setting affect variabilities of instantaneous sea surface height (ISSH) concering to one of the sea reference surface i.e mean sea surface height (MSSH). The differences between both heights, known as sea level anomaly (SLA), can be recognized as one of the parameter that describes the dynamic phenomena of the ocean. We investigated the Spatiotemporal characteristics of long-term SLA in this research based on 30 years of sea-level data derived from the multi-mission of satellite Altimetry (Topex/Poseidon, Jason-1, Jason-2 and Jason-3). The Spatiotemporal of SLA characteristics in Indonesian waters indicate substantial variations due to the influences of geographical location, bathymetric depth, and seasonal patterns. The SLA rate in the Indonesian region provides values that vary between 3.4 mm/yr to 5.3 mm/yr that higher than 3.2 mm/yr global SLA rate. The impact caused by the phenomenon needs to be taken into account given the vulnerability and disaster that could endanger the islands and coastal area in Indonesia. <strong></strong></p>

PREDICTING TIDAL MARSH SURVIVAL OR SUBMERGENCE TO FUTURE SEA-LEVEL RISE USING PALEO SEA-LEVEL DATA

2018 ◽  
Author(s):  
Benjamin P. Horton ◽  
◽  
Ian Shennan ◽  
Sarah L. Bradley ◽  
Niamh Cahill ◽  
...  
Keyword(s):  
Sea Level Rise ◽  
Sea Level ◽  
Tidal Marsh ◽  
Level Data

Validation and application of model/reanalysis sea-level data to the establishment of the reference hydrographic surface in Spanish waters

2021 ◽  
pp. 1-20
Author(s):  
Carlos J. González ◽  
J. Ramón Torres ◽  
Patricia Bernárdez ◽  
Rodolfo J. Ramos
Keyword(s):  
Sea Level ◽  
Level Data

Sea Surface Heights and Marine Gravity Determined from SARAL/AltiKa Ka-band Altimeter Over South China Sea

2021 ◽  
Author(s):  
Chengcheng Zhu ◽  
Xin Liu ◽  
Jinyun Guo ◽  
Shengwen Yu ◽  
Yupeng Niu ◽  
...  
Keyword(s):  
South China Sea ◽  
South China ◽  
Sea Surface ◽  
Ka Band ◽  
China Sea ◽  
Marine Gravity ◽  
Sea Surface Heights

scholarly journals Resolving discrepancies between field and modelled relative sea-level data: lessons from western Ireland

2017 ◽  
Vol 32 (7) ◽  
pp. 957-975 ◽  
Author(s):  
Robin Edwards ◽  
W. Roland Gehrels ◽  
Anthony Brooks ◽  
Ralph Fyfe ◽  
Katie Pullen ◽  
...  
Keyword(s):  
Sea Level ◽  
Relative Sea Level ◽  
Level Data ◽  
Western Ireland

Observations of postglacial uplift at Churchill, Manitoba

1992 ◽  
Vol 29 (11) ◽  
pp. 2418-2425 ◽  
Author(s):  
A. Mark Tushingham
Keyword(s):  
Sea Level ◽  
Tide Gauge ◽  
Ice Sheet ◽  
Laurentide Ice Sheet ◽  
Glacial Isostatic Adjustment ◽  
Tide Gauge Record ◽  
Isostatic Adjustment ◽  
Absolute Gravimetry ◽  
The Earth ◽  
Level Data

Churchill, Manitoba, is located near the centre of postglacial uplift caused by the Earth's recovery from the melting of the Laurentide Ice Sheet. The value of present-day uplift at Churchill has important implications in the study of postglacial uplift in that it can aid in constraining the thickness of the ice sheet and the rheology of the Earth. The tide-gauge record at Churchill since 1940 is examined, along with nearby Holocene relative sea-level data, geodetic measurements, and recent absolute gravimetry measurements, and a present-day rate of uplift of 8–9 mm/a is estimated. Glacial isostatic adjustment models yield similar estimates for the rate of uplift at Churchill. The effects of the tide-gauge record of the diversion of the Churchill River during the mid-1970's are discussed.

Airborne measurement of absolute sea-surface heights

1993 ◽  
Vol 20 (9) ◽  
pp. 875-878 ◽  
Author(s):  
John M. Brozena ◽  
Mary F. Peters ◽  
Rene Forsberg
Keyword(s):  
Sea Surface ◽  
Airborne Measurement ◽  
Sea Surface Heights
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