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salinity, and monsoon linkage: Variations in the Indian summer monsoons produce dramatic changes in sea surface salinity (hereafter salinity) structure because the salinity adjustment between the high-salinity Arabian Sea and low-salinity BOB largely depends upon the seasonally reversing monsoon sys
| Content Provider | Semantic Scholar |
|---|---|
| Copyright Year | 2014 |
| Abstract | 2 -1.4 6. Discussion In this section, sedimentary responses of the Holocene-Glacial period are presented first, as this record is available for all the three sediment cores, followed by the discussion on long-term responses based on the two deep-water cores (GC08 & CR04). As mentioned in the previous section, the multi-proxy data of the GC08 core are considered as the central evidences for the cumulative response of the EAS to climate change. The emphasis is given on themes of coupled responses rather than discussing each core individually based on each proxy, as the present cores provide an opportunity for a comprehensive understanding of changes in the entire EAS. The relevant data is provided at the end as Appendix. To extract the information on past changes in local E-P or salinity, the 8 180-correction required for subtracting the global ice-volume (or global sea level) effect from the composite calcite-8180, the presently available most precise sea level reconstruction by Shackleton (2000) (Figure 17) has been used. |
| File Format | PDF HTM / HTML |
| Alternate Webpage(s) | http://shodhganga.inflibnet.ac.in:8080/jspui/bitstream/10603/35670/14/14_chapter%206.pdf |
| Language | English |
| Access Restriction | Open |
| Content Type | Text |
| Resource Type | Article |
