Sci. Lett. 387, 27–33 (2014) ADS CAS Google Scholar Dutton, A. et al. Sea-level rise due to polar ice-sheet mass loss during past warm periods. Science 3491, http://dx.doi.org/10.1126/science.aaa4019 (2015) Kopp, R. E., Simons, F. J., Mitrovica, J. X., Maloof, A. ...
Ground surface temperatures, reconstructed from deep borehole temperature gradients, have increased by up to 4掳C in the past centuries and have been ... Zhang,Tingjun - 《Reviews of Geophysics》 被引量: 850发表: 2005年 Temperature trends over the past five centuries reconstructed from borehole...
Because the caves hosting POS are proximal to the coastline (within 300 m), the hydraulic gradient between them and the Mediterranean Sea is insignificant, thus, the brackish water table in these caves is today, and was in the past, coincident with sea level. As long as sea level remains ...
In particular, this paper aims to provide a step-wise decision process required to develop a more accurate forecasting model over short- and mid-term horizons. This work integrates variational mode decomposition (VMD) and bidirectional long short-term memory (BiLSTM) for multi-input multi-output ...
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De Lange and Carter analyse the causes of sea-level change, and describe how it has been measured – with tide gauges over the past 100 to 150 years and from satellites over the past 30 years. Their key message is to recall that sea-level change is a local phenomenon, with high ...
2014). These regional changes are shown to be associated with basin-wide spatial patterns, which exhibit distinct decadal variations (e.g., Lee and McPhaden 2008). For simplicity, in this paper “decadal variability” is collectively referred to as variations from one to a few decades (...
A refined relative sea level (RSL) history spanning the past 14,300 calendar years is described for the Quadra Island area in the northern Strait of Georgia on the Pacific coast of Canada. Here marine shorelines dating to the time of earliest post-glacial emergence are at least 197 m abo...
Recently published estimates of continental glaciers melting, ice sheets melting and land water mass change suggest that the latter sources have contributed to about 1 mm/yr eustatic (i.e., non steric) sea level rise during the past decade. This raises a new enigma: since Topex-derived sea ...
Our palaeoclimate reconstructions indicate that the transition occurred either as a predominantly abrupt shift towards the end of the LIA, or as a more gradual, continued decline over the past 150 years; this ambiguity probably arises from non-AMOC influences on the various proxies or from the ...