Global sea level change signatures observed by GRACE satellite gravimetry

Ice mass loss on land results in sea level rise, but its rate varies regionally due to gravitational self-attraction effects. Observing regional sea level rates by ocean mass change using the Gravity Recovery and Climate Experiment (GRACE) gravity solutions is difficult due to GRACE’s spatial resolu...

Descripción completa

Detalles Bibliográficos
Autores principales: Jeon, Taehwan, Seo, Ki-Weon, Youm, Kookhyoun, Chen, Jianli, Wilson, Clark R.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6131218/
https://www.ncbi.nlm.nih.gov/pubmed/30202083
http://dx.doi.org/10.1038/s41598-018-31972-8

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6131218/
https://www.ncbi.nlm.nih.gov/pubmed/30202083
http://dx.doi.org/10.1038/s41598-018-31972-8

Ejemplares similares