The absence of large negative anomalies in the 1990s for
the annual WAIS timeseries implies that the sign of the temperature trend for WAIS is less sensitive to start dates of the analysis than for EAIS and all Antarctica.
The annual WAIS Divide Ice Core scientific meeting unfolds over two days at a Sheraton less than a mile from the ice core lab.
Walter, J., Peng, Z., Aster, R., Wiens, D., Anandakrishnan, S., Nyblade, A., Triggering of icequake seismicity throughout Antarctica, 20th
Annual WAIS Workshop, Sterling, VA, 29 September - 2 October, 2013.
Lloyd, A., Wiens, D., Shore, P., Nyblade, A., Anandakrishnan, S., Aster, R., Huerta, A., Wilson, T., Zhao, D., West Antarctica Ice Sheet Upper Mantle Structure Beneath the Whitmore Mountains, West Antarctic Rift System, and Marie Byrd Land from Body Wave Tomography, Eighteenth
annual WAIS workshop, Loveland, CO, 21 - 23 September, 2011.
Not exact matches
A 420 Year
Annual 10Be Record from the
WAIS Divide Ice Core.
Comparing the
annual timeseries (Fig. 2), the EAIS and
WAIS timeseries are similar from the 1960s through the 1980s, but show differences in the 1990s.
All four of the datasets indicate that the spring and
annual warming rates are slightly larger for the WA than the
WAIS domain, while the winter warming trend is not statistically significant in the WA domain.
Timeseries of Antarctic temperature anomalies from the M10, STEIGv1, and CHAPMAN datasets, for the
annual mean (left column) and spring (SON, right column), and aggregated for ALL Antarctica (top row), EAIS (middle row) and
WAIS (bottom row)
The average central trend estimate of the four datasets for
WAIS is 0.18 °C / decade for the
annual mean.