Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Closing the global mean sea level budget from altimetry, GRACE/GRACE Follow-On and Argo data (2005-present)

View through CrossRef
<p>Change in the global mean sea level (GMSL) is the sum of changes in the global mean steric sea level and global mean ocean mass. Over the 1993-2016 period, the GMSL budget was found to be closed, as shown by many independent studies. However, non-closure of the sea level budget after 2016 has been recently reported when using altimetry, Argo and GRACE/GRACE Follow-On data (Chen et al., GRL, 2020). This non-closure may result from errors in one or more components of the sea level budget (altimetry-based GMSL, Argo-based steric sea level or GRACE-based ocean mass). In this study, we investigated possible sources of errors affecting atlimetry and Argo data used to assess closure of the GMSL budget. Concerning altimetry data, we compared the wet tropospheric correction (WTC) applied to Jason-3 data (the reference satellite mission used for the GMSL computation since 2016) with that from the SARAL/AltiKa mission, and found no systematic bias between the radiometer measurements from these two missions. Besides, preliminary comparisons of GMSL trends (using the WTC ECMWF model) between different missions do not suggest discrepancies larger than 0.4 mm/yr over 2016-present. While further analyses are still needed, we find unlikely that non-closure of the sea level budget results from errors of the altimetry system. Concerning Argo data, since 2016, salinity data from different processing groups display strong discrepancies, likely due to instrumental problems and data editing issues. Good agreement is found between all available Argo-based thermosteric products. Given that the halosteric component should be negligible in global average, we re-examined the sea level budget since 2016 using only the thermosteric component and found significant improvement in the budget closure, although it is not yet fully closed. This suggests that the observed discrepancies in the Argo-based halosteric component largely contribute to the non-closure of the GMSL budget in the recent years.</p>
Title: Closing the global mean sea level budget from altimetry, GRACE/GRACE Follow-On and Argo data (2005-present)
Description:
<p>Change in the global mean sea level (GMSL) is the sum of changes in the global mean steric sea level and global mean ocean mass.
Over the 1993-2016 period, the GMSL budget was found to be closed, as shown by many independent studies.
However, non-closure of the sea level budget after 2016 has been recently reported when using altimetry, Argo and GRACE/GRACE Follow-On data (Chen et al.
, GRL, 2020).
This non-closure may result from errors in one or more components of the sea level budget (altimetry-based GMSL, Argo-based steric sea level or GRACE-based ocean mass).
In this study, we investigated possible sources of errors affecting atlimetry and Argo data used to assess closure of the GMSL budget.
Concerning altimetry data, we compared the wet tropospheric correction (WTC) applied to Jason-3 data (the reference satellite mission used for the GMSL computation since 2016) with that from the SARAL/AltiKa mission, and found no systematic bias between the radiometer measurements from these two missions.
Besides, preliminary comparisons of GMSL trends (using the WTC ECMWF model) between different missions do not suggest discrepancies larger than 0.
4 mm/yr over 2016-present.
While further analyses are still needed, we find unlikely that non-closure of the sea level budget results from errors of the altimetry system.
Concerning Argo data, since 2016, salinity data from different processing groups display strong discrepancies, likely due to instrumental problems and data editing issues.
Good agreement is found between all available Argo-based thermosteric products.
Given that the halosteric component should be negligible in global average, we re-examined the sea level budget since 2016 using only the thermosteric component and found significant improvement in the budget closure, although it is not yet fully closed.
This suggests that the observed discrepancies in the Argo-based halosteric component largely contribute to the non-closure of the GMSL budget in the recent years.
</p>.

Related Results

Analisis Konsumsi Daya Listrik Pada Kereta Penumpang Kelas Eksekutif Argo Cirebon (Studi Pada PT. Kereta Api Indonesia Daop 1 Jakarta)
Analisis Konsumsi Daya Listrik Pada Kereta Penumpang Kelas Eksekutif Argo Cirebon (Studi Pada PT. Kereta Api Indonesia Daop 1 Jakarta)
ABSTRACT The purpose of this study is to conduct a study of the total electricity consumption on the Argo Cirebon executive class train, and to find out the number of passeng...
Revisiting the global mean ocean mass budget over 2005-202
Revisiting the global mean ocean mass budget over 2005-202
We investigate the performances of GRACE and GRACE Follow-On satellite gravimetry missions in assessing the ocean mass budget at global scale over 2005-2020. For that purpose, we f...
Global Sea Level Budget 1993–Present
Global Sea Level Budget 1993–Present
Abstract. Global mean sea level is an integral of changes occurring in the climate system in response to unforced climate variability as well as natural and anthropogenic forcing f...
Lagrangian measurements in the West Spitsbergen Current by Argo floats
Lagrangian measurements in the West Spitsbergen Current by Argo floats
<p>Almost 4000 operational Argo floats covering the world's ocean provide near-real-time data on its state. The Arctic is less covered than other waters, but observat...
Global mean and local sea level budget from updated observations and residual analysis
Global mean and local sea level budget from updated observations and residual analysis
The closure of the Sea Level Budget (SLB) is a key challenge for modern physical oceanography. First, it is essential that we ensure the proper identification and quantification of...
Intraseasonal Variability in the Persian Gulf Revealed by GRACE and Altimetry
Intraseasonal Variability in the Persian Gulf Revealed by GRACE and Altimetry
<p>The Persian Gulf is a semi-enclosed marginal sea of the Indian Ocean. It connects to the Arabian Sea through the Gulf of Oman and the Strait of Hormuz. The Persian...
Altimetry Waveform Classification and Retracking Strategy for Improved Coastal Altimetry Products
Altimetry Waveform Classification and Retracking Strategy for Improved Coastal Altimetry Products
Coastal zones exhibit unique altimetry signal characteristics, primarily influenced by the presence of land artifacts. The shape of the altimetry echo serves as a distinctive marke...
Regionalizing the Sea-level Budget Using a Neural Network Approach
Regionalizing the Sea-level Budget Using a Neural Network Approach
<p><span>Understanding the drivers of present-day sea-level change is vital for improving sea-level projections and for adaptation and mitigation plans ...

Back to Top