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Estimating the sources of global sea level rise with data assimilation techniques
A rapidly melting ice sheet produces a distinctive geometry, or fingerprint, of sea level (SL) change. Thus, a network of SL observations may, in principle, be used to infer sources of meltwater flux. We outline a formalism, based on a modified Kalman smoother, for using tide gauge observations to e...
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| Hlavní autoři: | , , , |
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| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
National Academy of Sciences
2013
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3586610/ https://ncbi.nlm.nih.gov/pubmed/22543163 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1117683109 |
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