Climate warming in polar regions is associated with thawing of permafrost, resulting in significant changes in soil hydrology, biogeochemical cycling, and in the activity and composition of soil communities. While ongoing directional climate warming presses can elicit such responses over decadal time scales, their manifestation typically occurs as discrete thawing pulses. Indeed, in the McMurdo Dry Valleys of Antarctica, abrupt changes in community structure and biogeochemical cycling in terrestrial and aquatic ecosystems following a summer warming event (Jan.
Dataset Results
2012-01-08 to 2021-12-03
10.6073/pasta/b144efdd5592d4a98ee28a0a258d8fd1
4017
As part of the McMurdo Dry Valleys Long Term Ecological Research program, meteorological data are collected from various locations throughout the McMurdo Dry Valleys of Antarctica. This data package contains 15-minute data from the Miers Valley Meteorological Station (MISM), located in Miers Valley.
Date Range:
2012-01-28 to 2022-12-18
Data sources:
DOI:
10.6073/pasta/07ddf8aa9be93d8071326c34697bb56b
Dataset ID:
7020
As part of the McMurdo Dry Valleys Long Term Ecological Research program, meteorological data are collected from various locations throughout the McMurdo Dry Valleys of Antarctica. This data package contains daily measurement summaries derived from 15-minute data generated by the Miers Valley Meteorological Station (MISM), located in Miers Valley.
Date Range:
2012-01-28 to 2022-12-18
Data sources:
DOI:
10.6073/pasta/a6869b69f5ca60f161f051c62c23394d
Dataset ID:
7120