38 citations as recorded by crossref.

1. Multidecadal variations in Southern Hemisphere atmospheric 14C: Evidence against a Southern Ocean sink at the end of the Little Ice Age CO2 anomaly C. Turney et al. 10.1002/2015GB005257
2. The Antarctic Centennial Oscillation: A Natural Paleoclimate Cycle in the Southern Hemisphere That Influences Global Temperature W. Davis et al. 10.3390/cli6010003
3. Evidence for increased expression of the Amundsen Sea Low over the South Atlantic during the late Holocene Z. Thomas et al. 10.5194/cp-14-1727-2018
4. The Origin and Propagation of the Antarctic Centennial Oscillation W. Davis et al. 10.3390/cli7090112
5. Evidence for a floristically diverse rainforest on the Falkland archipelago in the remote South Atlantic during the mid- to late Cenozoic Z. Thomas et al. 10.1017/S0954102024000129
6. Pollen evidence of variations in Holocene climate and Southern Hemisphere Westerly Wind strength on sub-Antarctic South Georgia M. Zwier et al. 10.1177/09596836211060495
7. A pre-European archaeology in Malvinas/Falkland Islands? A review A. Zangrando & L. Borrero 10.1080/15564894.2022.2077484
8. The role of Southern Hemispheric Westerlies for Holocene hydroclimatic changes in the steppe of Tierra del Fuego (Argentina) C. Laprida et al. 10.1016/j.quaint.2020.09.051
9. Southern Hemisphere Westerly Winds have modulated the formation of laminations in sediments in Lago Fagnano (Tierra del Fuego, Argentina) over the past 6.3 ka A. Vizcaino et al. 10.1111/bor.12600
10. Anomalous mid-twentieth century atmospheric circulation change over the South Atlantic compared to the last 6000 years C. Turney et al. 10.1088/1748-9326/11/6/064009
11. Holocene dynamics of the Southern Hemisphere westerly winds and possible links to CO2 outgassing K. Saunders et al. 10.1038/s41561-018-0186-5
12. Ecology of moss banks on Signy Island (maritime Antarctic) N. Cannone et al. 10.1093/botlinnean/box040
13. Holocene glacier fluctuations and environmental changes in subantarctic South Georgia inferred from a sediment record from a coastal inlet S. Berg et al. 10.1017/qua.2018.85
14. Regional validation of the use of diatoms in ice cores from the Antarctic Peninsula as a Southern Hemisphere westerly wind proxy D. Tetzner et al. 10.5194/cp-18-1709-2022
15. The Falkland Islands’ palaeoecological response to millennial‐scale climate perturbations during the Pleistocene–Holocene transition: Implications for future vegetation stability in the southern ocean islands R. Scaife et al. 10.1002/jqs.3150
16. Late Holocene intensification of the westerly winds at the subantarctic Auckland Islands (51° S), New Zealand I. Browne et al. 10.5194/cp-13-1301-2017
17. Reduced rainfall drives biomass limitation of long‐term fire activity in Australia’s subtropical sclerophyll forests M. Mariani et al. 10.1111/jbi.13628
18. Late Glacial and Holocene Palaeolake History of the Última Esperanza Region of Southern Patagonia S. Roberts et al. 10.3389/feart.2022.813396
19. Sea surface temperature in the Indian sector of the Southern Ocean over the Late Glacial and Holocene L. Orme et al. 10.5194/cp-16-1451-2020
20. Investigating Subantarctic14C Ages of Different Peat Components: Site and Sample Selection for Developing Robust Age Models in Dynamic Landscapes Z. Thomas et al. 10.1017/RDC.2019.54
21. Reconstructing atmospheric circulation over southern New Zealand: Establishment of modern westerly airflow 5500 years ago and implications for Southern Hemisphere Holocene climate change C. Turney et al. 10.1016/j.quascirev.2016.12.017
22. Holocene changes in the position of the Southern Hemisphere Westerlies recorded by long-distance transport of pollen to the Kerguelen Islands M. Zwier et al. 10.1016/j.quascirev.2024.108595
23. Solar Output Controls Periodicity in Lake Productivity and Wetness at Southernmost South America M. Pérez-Rodríguez et al. 10.1038/srep37521
24. Tracing last millennium cycles of Río de la Plata Plume Water input into the Southwestern Atlantic Ocean L. Perez et al. 10.1016/j.scitotenv.2023.166680
25. Solar irradiance and primary productivity controlled mercury accumulation in sediments of a remote lake in the Southern Hemisphere during the past 4000 years H. Biester et al. 10.1002/lno.10647
26. Seabird establishment during regional cooling drove a terrestrial ecosystem shift 5000 years ago D. Groff et al. 10.1126/sciadv.abb2788
27. Evidence of prehistoric human activity in the Falkland Islands K. Hamley et al. 10.1126/sciadv.abh3803
28. Mid-Holocene intensification of Southern Hemisphere westerly winds and implications for regional climate dynamics J. Tamhane et al. 10.1016/j.quascirev.2023.108007
29. A New Zealand perspective on centennial-scale Southern Hemisphere westerly wind shifts during the last two millennia J. Hinojosa et al. 10.1016/j.quascirev.2017.07.016
30. Falkland Island peatland development processes and the pervasive presence of fire D. Mauquoy et al. 10.1016/j.quascirev.2020.106391
31. Distal ash fall from the mid-Holocene eruption of Mount Hudson (H2) discovered in the Falkland Islands: New possibilities for Southern Hemisphere archive synchronisation P. Panaretos et al. 10.1016/j.quascirev.2021.107074
32. Holocene centennial to millennial shifts in North-Atlantic storminess and ocean dynamics J. Goslin et al. 10.1038/s41598-018-29949-8
33. The Medieval Climate Anomaly in Antarctica S. Lüning et al. 10.1016/j.palaeo.2019.109251
34. Tracking the southern hemisphere westerlies during and since the last glacial maximum with multiproxy lake records from the Falkland Islands (52 °S) M. Spoth et al. 10.1016/j.quascirev.2023.108135
35. Late Holocene climate anomaly concurrent with fire activity and ecosystem shifts in the eastern Australian Highlands Z. Thomas et al. 10.1016/j.scitotenv.2021.149542
36. 17,000 years of vegetation, fire and climate change in the eastern foothills of the Andes (lat. 44°S) V. Iglesias et al. 10.1016/j.palaeo.2016.06.008
37. The Medieval Climate Anomaly in South America S. Lüning et al. 10.1016/j.quaint.2018.10.041
38. Intensification of Southern Hemisphere westerly winds 2000–1000 years ago: evidence from the subantarctic Campbell and Auckland Islands (52–50°S) C. Turney et al. 10.1002/jqs.2828