62 citations as recorded by crossref.

1. Ice-sheet configuration in the CMIP5/PMIP3 Last Glacial Maximum experiments A. Abe-Ouchi et al. 10.5194/gmd-8-3621-2015
2. Back to the Future: Using Long-Term Observational and Paleo-Proxy Reconstructions to Improve Model Projections of Antarctic Climate T. Bracegirdle et al. 10.3390/geosciences9060255
3. Simulated Southern Ocean Upwelling at the Last Glacial Maximum and Early Deglaciation: The Role of Eddy‐Induced Overturning Circulation C. Chen & G. Wang 10.1029/2021GL092880
4. Understanding the Uncertainty in the 21st Century Dynamic Sea Level Projections: The Role of the AMOC C. Chen et al. 10.1029/2018GL080676
5. Hydrographic changes in the Agulhas Recirculation Region during the late Quaternary D. Naik et al. 10.5194/cp-10-745-2014
6. South African winter rainfall zone shifts: A comparison of seasonality metrics for Cape Town from 1841–1899 and 1933–2020 S. Roffe et al. 10.1007/s00704-021-03911-7
7. Influence of glacial ice sheets on the Atlantic meridional overturning circulation through surface wind change S. Sherriff-Tadano et al. 10.1007/s00382-017-3780-0
8. Southern African precipitation changes in a warmer world: insights from the PlioMIP2 mid-Pliocene warm period (∼3.3–3.0 Ma) ensemble S. Roffe et al. 10.1080/0035919X.2024.2410945
9. Changes in the position of the Subtropical Front south of New Zealand since the last glacial period H. Bostock et al. 10.1002/2014PA002652
10. Holocene dynamics of the Southern Hemisphere westerly winds and possible links to CO2 outgassing K. Saunders et al. 10.1038/s41561-018-0186-5
11. Investigating monthly geopotential height changes and mid-latitude Northern Hemisphere westerlies H. Asakereh et al. 10.1007/s00704-024-04879-w
12. Northern Westerlies during the Last Glacial Maximum: Results from CMIP5 Simulations N. Wang et al. 10.1175/JCLI-D-17-0314.1
13. High mid-Holocene accumulation rates over West Antarctica inferred from a pervasive ice-penetrating radar reflector J. Bodart et al. 10.5194/tc-17-1497-2023
14. Climate history of the Southern Hemisphere Westerlies belt during the last glacial–interglacial transition revealed from lake water oxygen isotope reconstruction of Laguna Potrok Aike (52° S, Argentina) J. Zhu et al. 10.5194/cp-10-2153-2014
15. Poleward Shift in the Southern Hemisphere Westerly Winds Synchronous With the Deglacial Rise in CO2 W. Gray et al. 10.1029/2023PA004666
16. Evaluation of CMIP5 palaeo-simulations to improve climate projections S. Harrison et al. 10.1038/nclimate2649
17. Mechanisms of millennial-scale atmospheric CO2 change in numerical model simulations J. Gottschalk et al. 10.1016/j.quascirev.2019.05.013
18. Variability of surface climate in simulations of past and future K. Rehfeld et al. 10.5194/esd-11-447-2020
19. The Southern Ocean during the ice ages: A review of the Antarctic surface isolation hypothesis, with comparison to the North Pacific D. Sigman et al. 10.1016/j.quascirev.2020.106732
20. How might the North American ice sheet influence the northwestern Eurasian climate? P. Beghin et al. 10.5194/cp-11-1467-2015
21. Widening of the Hadley Cell from Last Glacial Maximum to Future Climate S. Son et al. 10.1175/JCLI-D-17-0328.1
22. Proxy‐Based Preformed Phosphate Estimates Point to Increased Biological Pump Efficiency as Primary Cause of Last Glacial Maximum CO2 Drawdown T. Vollmer et al. 10.1029/2021PA004339
23. What drives LGM precipitation over the western Mediterranean? A study focused on the Iberian Peninsula and northern Morocco P. Beghin et al. 10.1007/s00382-015-2720-0
24. Bottom current control on sediment deposition between the Iselin Bank and the Hillary Canyon (Antarctica) since the late Miocene: An integrated seismic-oceanographic approach R. Conte et al. 10.1016/j.dsr.2021.103606
25. Mid-Pliocene westerlies from PlioMIP simulations X. Li et al. 10.1007/s00376-014-4171-7
26. CMIP5 Diversity in Southern Westerly Jet Projections Related to Historical Sea Ice Area: Strong Link to Strengthening and Weak Link to Shift T. Bracegirdle et al. 10.1175/JCLI-D-17-0320.1
27. Hydrogen and carbon isotope fractionation in modern plant wax n-alkanes from the Falkland Islands M. Corcoran et al. 10.1016/j.orggeochem.2022.104404
28. Effect of Upper- and Lower-Level Baroclinicity on the Persistence of the Leading Mode of Midlatitude Jet Variability L. Robert et al. 10.1175/JAS-D-18-0010.1
29. Deglacial weakening of the oceanic soft tissue pump: global constraints from sedimentary nitrogen isotopes and oxygenation proxies E. Galbraith & S. Jaccard 10.1016/j.quascirev.2014.11.012
30. Long-term changes in the speed and direction of westerlies in the mid-latitudes of the Northern Hemisphere (MLNH) H. Asakereh & A. Jahedi 10.1007/s11600-024-01525-x
31. Last Glacial Maximum climate and atmospheric circulation over the Australian region from climate models Y. Du et al. 10.5194/cp-20-393-2024
32. Southern Hemisphere westerlies as a driver of the early deglacial atmospheric CO2 rise L. Menviel et al. 10.1038/s41467-018-04876-4
33. The Driving Mechanisms on Southern Ocean Upwelling Change during the Last Deglaciation W. Liu et al. 10.3390/geosciences11070266
34. Changes in latitudinal sea surface temperature gradients along the Southern Chilean margin since the last glacial N. Haddam et al. 10.1016/j.quascirev.2018.06.023
35. Breakdown of the Linear Relationship between the Southern Hemisphere Hadley Cell Edge and Jet Latitude Changes in the Last Glacial Maximum S. Kim & S. Son 10.1175/JCLI-D-19-0531.1
36. Modeling Obliquity and CO2 Effects on Southern Hemisphere Climate during the Past 408 ka* A. Timmermann et al. 10.1175/JCLI-D-13-00311.1
37. Downscaling Last Glacial Maximum climate over southern Africa F. Engelbrecht et al. 10.1016/j.quascirev.2019.105879
38. Variability of the Southwestern Patagonia (51°S) Winds in the Recent (1980–2020) Period: Implications for Past Wind Reconstructions C. Gómez-Fontealba et al. 10.3390/atmos13020206
39. The Roles of Orbital and Meltwater Climate Forcings on the Southern Ocean Dynamics during the Last Deglaciation G. Mandal et al. 10.3390/su14052927
40. The ‘Day Zero’ Cape Town drought and the poleward migration of moisture corridors P. Sousa et al. 10.1088/1748-9326/aaebc7
41. The Impact of Incomplete Nutrient Consumption in the Southern Ocean on Global Mean Ocean Nitrate δ15N F. Fripiat et al. 10.1029/2022GB007442
42. Two AMOC States in Response to Decreasing Greenhouse Gas Concentrations in the Coupled Climate Model MPI-ESM M. Klockmann et al. 10.1175/JCLI-D-17-0859.1
43. Historically-based run-time bias corrections substantially improve model projections of 100 years of future climate change G. Krinner et al. 10.1038/s43247-020-00035-0
44. Shifting frontal regimes and its influence on bioproductivity variations during the Late Quaternary in the Indian sector of Southern Ocean M. Manoj & M. Thamban 10.1016/j.dsr2.2015.03.011
45. Impacts of the PMIP4 ice sheets on Northern Hemisphere climate during the last glacial period K. Izumi et al. 10.1007/s00382-022-06456-1
46. Sea ice led to poleward-shifted winds at the Last Glacial Maximum: the influence of state dependency on CMIP5 and PMIP3 models L. Sime et al. 10.5194/cp-12-2241-2016
47. Summer Westerly Jet in Northern Hemisphere during the Mid-Holocene: A Multi-Model Study C. Xu et al. 10.3390/atmos11111193
48. Global monsoon change during the Last Glacial Maximum: a multi-model study M. Yan et al. 10.1007/s00382-015-2841-5
49. The de-correlation of westerly winds and westerly-wind stress over the Southern Ocean during the Last Glacial Maximum W. Liu et al. 10.1007/s00382-015-2530-4
50. Steering of westerly storms over western North America at the Last Glacial Maximum J. Oster et al. 10.1038/ngeo2365
51. Inter-model diversity in jet stream changes and its relation to Arctic climate in CMIP5 B. Yim et al. 10.1007/s00382-015-2833-5
52. Southern ocean response to glacial and interglacial forcing N. Leonardo et al. 10.1016/j.jsames.2023.104642
53. Evolution of the meridional shift of the subtropical and subpolar westerly jet over the Southern Hemisphere during the past 21,000 years N. Jiang & Q. Yan 10.1016/j.quascirev.2020.106544
54. Asymmetry of hemispheric climate during MIS 16 versus MIS 12 X. Ma et al. 10.1016/j.quascirev.2024.108721
55. South Pacific Subtropical High from the late Holocene to the end of the 21st century: insights from climate proxies and general circulation models V. Flores-Aqueveque et al. 10.5194/cp-16-79-2020
56. Sensitivity of southern hemisphere westerly wind to boundary conditions for the last glacial maximum S. Kim et al. 10.1016/j.quaint.2017.04.001
57. Cyclostratigraphic studies of sediments from Lake Van (Turkey) based on their uranium contents obtained from downhole logging and paleoclimatic implications H. Baumgarten & T. Wonik 10.1007/s00531-014-1082-x
58. Investigating changes in rainfall seasonality across South Africa: 1987–2016 S. Roffe et al. 10.1002/joc.6830
59. Wind-driven changes in Southern Ocean residual circulation, ocean carbon reservoirs and atmospheric CO2 J. Lauderdale et al. 10.1007/s00382-012-1650-3
60. Sensitivity of Southern Hemisphere circulation to LGM and 4 × CO2 climates M. Rojas 10.1002/grl.50195
61. Computation of rare transitions in the barotropic quasi-geostrophic equations J. Laurie & F. Bouchet 10.1088/1367-2630/17/1/015009
62. Poleward and weakened westerlies during Pliocene warmth J. Abell et al. 10.1038/s41586-020-03062-1