A New Zealand perspective on centennial-scale Southern Hemisphere westerly wind shifts during the last two millennia

摘要

Abstract The strength and latitudinal position of the Southern Hemisphere westerly winds control regional climate and influence the global carbon cycle by physically regulating Southern Ocean CO2 exchange with the atmosphere. However, the mechanisms driving interannual to millennial variability of the westerlies remain poorly understood. Here, we present an 1800-yr record of westerly wind variability recorded in New Zealand fjord sediments. Located west of the Southern Alps, fjord basins receive large amounts of westerly-driven orographic precipitation (6?m?yr?1) and strong winds lead to vigorous fjord mixing. Because of these links, reconstructing precipitation and fjord circulation provides information on westerly wind behavior over southwest New Zealand. Applying a multiproxy approach, we find several intervals of inferred regional wind variability. The intervals of 1450-1400, 825-775, 575-550, and 50-0?cal?yr BP were anomalously wet, while 325-300 and 250-225?cal?yr BP were anomalously dry. These interpreted intervals appear to be in phase with regional paleoclimate records. Two centennial-scale wet intervals align with a multi-centennial warm interval identified in the Pages2k Australasian temperature reconstruction, while the drier intervals generally occur during cooler times. The wet/dry intervals presented here are matched by opposite wind and/or precipitation trends reconstructed from the windfield core in Chile and the southern windfield margin in Antarctica. Such spatial patterns support the notion of centennial-scale latitudinal wind shifts or contraction/expansion of the core. Consistent with observations, all sites show wind strengthening from ～50?cal?yr BP to present, indicating an overall intensification of winds that is observed in modern instrumental and reanalysis data sets. Highlights ? A 2-kyr New Zealand sediment core records centennial-scale westerly wind variability. ? A strong peak in wind-driven precipitation occurs at 800?cal?yr BP. ? Reconstructions from similar latitudes across the Pacific show divergent trends. ]]>