Clémence Chupin, V. Ballu, L. Testut, Y. Tranchant, J. Aucan
{"title":"Nouméa: a new multi-mission calibration and validation site for past and future altimetry missions?","authors":"Clémence Chupin, V. Ballu, L. Testut, Y. Tranchant, J. Aucan","doi":"10.5194/os-19-1277-2023","DOIUrl":null,"url":null,"abstract":"Abstract. Today, monitoring the evolution of sea level in coastal\nareas is of importance, since almost 11 % of the world's population\nlives\nin low-lying areas. Reducing uncertainties in sea level estimates requires\na\nbetter understanding of both altimetry measurements and local sea level\ndynamics. In New Caledonia, the Nouméa lagoon is an example of this\nchallenge, as altimetry, coastal tide gauge, and vertical land motions\nfrom global navigation satellite systems (GNSSs) do not provide consistent\ninformation. The GEOCEAN-NC 2019 field campaign addresses this issue with\ndeployments of in situ instruments in the lagoon (GNSS buoy,\npressure gauge, etc.),\nwith a particular focus on the crossover of one Jason-series track and two\nSentinel-3A missions tracks. In this study, we propose a method to\nvirtually\ntransfer the Nouméa tide gauge at the altimetry crossover point, using\nin situ data\nfrom the field campaign. Following the philosophy of calibration and validation (Cal/Val) studies, we\nderive absolute altimeter bias time series over the entire Jason and\nSentinel-3A periods. Overall, our estimated altimeter mean biases are\nslightly larger by 1–2 cm compared to Corsica and Bass Strait results,\nwith\ninter-mission biases in line with those of Bass Strait site. Uncertainties\nstill remain regarding the determination of our vertical datum, only\nconstrained by the three days of the GNSS buoy deployment. With our method,\nwe are able to re-analyse about 20 years of altimetry observations and\nderive a linear trend of −0.2 ± 0.1 mm yr−1 over the bias time series.\nCompared to previous studies, we do not find any significant uplift in the\narea, which is more consistent with the observations of inland permanent\nGNSS stations. These results support the idea of developing Cal/Val\nactivities in the lagoon, which is already the subject of several\nexperiments for the scientific calibration phase of the SWOT wide-swath\naltimetry mission.\n","PeriodicalId":19535,"journal":{"name":"Ocean Science","volume":"39 1","pages":""},"PeriodicalIF":4.1000,"publicationDate":"2023-08-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Ocean Science","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.5194/os-19-1277-2023","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"METEOROLOGY & ATMOSPHERIC SCIENCES","Score":null,"Total":0}
引用次数: 0
Abstract
Abstract. Today, monitoring the evolution of sea level in coastal
areas is of importance, since almost 11 % of the world's population
lives
in low-lying areas. Reducing uncertainties in sea level estimates requires
a
better understanding of both altimetry measurements and local sea level
dynamics. In New Caledonia, the Nouméa lagoon is an example of this
challenge, as altimetry, coastal tide gauge, and vertical land motions
from global navigation satellite systems (GNSSs) do not provide consistent
information. The GEOCEAN-NC 2019 field campaign addresses this issue with
deployments of in situ instruments in the lagoon (GNSS buoy,
pressure gauge, etc.),
with a particular focus on the crossover of one Jason-series track and two
Sentinel-3A missions tracks. In this study, we propose a method to
virtually
transfer the Nouméa tide gauge at the altimetry crossover point, using
in situ data
from the field campaign. Following the philosophy of calibration and validation (Cal/Val) studies, we
derive absolute altimeter bias time series over the entire Jason and
Sentinel-3A periods. Overall, our estimated altimeter mean biases are
slightly larger by 1–2 cm compared to Corsica and Bass Strait results,
with
inter-mission biases in line with those of Bass Strait site. Uncertainties
still remain regarding the determination of our vertical datum, only
constrained by the three days of the GNSS buoy deployment. With our method,
we are able to re-analyse about 20 years of altimetry observations and
derive a linear trend of −0.2 ± 0.1 mm yr−1 over the bias time series.
Compared to previous studies, we do not find any significant uplift in the
area, which is more consistent with the observations of inland permanent
GNSS stations. These results support the idea of developing Cal/Val
activities in the lagoon, which is already the subject of several
experiments for the scientific calibration phase of the SWOT wide-swath
altimetry mission.
期刊介绍:
Ocean Science (OS) is a not-for-profit international open-access scientific journal dedicated to the publication and discussion of research articles, short communications, and review papers on all aspects of ocean science: experimental, theoretical, and laboratory. The primary objective is to publish a very high-quality scientific journal with free Internet-based access for researchers and other interested people throughout the world.
Electronic submission of articles is used to keep publication costs to a minimum. The costs will be covered by a moderate per-page charge paid by the authors. The peer-review process also makes use of the Internet. It includes an 8-week online discussion period with the original submitted manuscript and all comments. If accepted, the final revised paper will be published online.
Ocean Science covers the following fields: ocean physics (i.e. ocean structure, circulation, tides, and internal waves); ocean chemistry; biological oceanography; air–sea interactions; ocean models – physical, chemical, biological, and biochemical; coastal and shelf edge processes; paleooceanography.