Format
Sort by
Items per page

Send to

Choose Destination

Search results

Items: 7

1.

Neodymium isotope evidence for glacial-interglacial variability of deepwater transit time in the Pacific Ocean.

Hu R, Piotrowski AM.

Nat Commun. 2018 Nov 9;9(1):4709. doi: 10.1038/s41467-018-07079-z.

2.

Atlantic deep water provenance decoupled from atmospheric CO2 concentration during the lukewarm interglacials.

Howe JNW, Piotrowski AM.

Nat Commun. 2017 Dec 8;8(1):2003. doi: 10.1038/s41467-017-01939-w.

3.

North Atlantic ocean circulation and abrupt climate change during the last glaciation.

Henry LG, McManus JF, Curry WB, Roberts NL, Piotrowski AM, Keigwin LD.

Science. 2016 Jul 29;353(6298):470-4. doi: 10.1126/science.aaf5529. Epub 2016 Jun 30.

4.

North Atlantic Deep Water Production during the Last Glacial Maximum.

Howe JN, Piotrowski AM, Noble TL, Mulitza S, Chiessi CM, Bayon G.

Nat Commun. 2016 Jun 3;7:11765. doi: 10.1038/ncomms11765.

5.

Evolution of ocean temperature and ice volume through the mid-Pleistocene climate transition.

Elderfield H, Ferretti P, Greaves M, Crowhurst S, McCave IN, Hodell D, Piotrowski AM.

Science. 2012 Aug 10;337(6095):704-9. doi: 10.1126/science.1221294.

6.

Synchronous deglacial overturning and water mass source changes.

Roberts NL, Piotrowski AM, McManus JF, Keigwin LD.

Science. 2010 Jan 1;327(5961):75-8. doi: 10.1126/science.1178068.

7.

Temporal relationships of carbon cycling and ocean circulation at glacial boundaries.

Piotrowski AM, Goldstein SL, Hemming SR, Fairbanks RG.

Science. 2005 Mar 25;307(5717):1933-8.

Supplemental Content

Loading ...
Support Center