However, firn diffusion smooths subannual signals, such that the shortest recoverable periodicity is generally no shorter than 1 year25,26. Such records were therefore annualized to a Jan-Dec window. The vast majority of records in the database are annually-resolved, and are not affected by ...
1). Based on marked differences in both the basement geology and sedimentary cover sequences, the Lhasa terrane can further be subdivided into the northern, central and southern sub-terranes, which are separated by the Shiquan River-Nam Tso mélange (SNMZ) and the Luobadui–Milashan fault (...
5, temperature reconstructions of the Common Era have become a key component of climate assessments6,7,8,9. Such reconstructions depend strongly on the composition of the underlying network of climate proxies10, and it is therefore critical for the climate community to have access to a community...
ovalis was of diuron. ~31 °C (fitted) while low and high temperatures There were significant interactions between the inhibited effects of t∆emF/pFem′raatsurdeidanadll diuron, with a majority of the combinations of these stressors causing sub-additive (antagonistic) effects. While the ...
India is a key global region vulnerable to climate change; however, limited studies have focused on the combine effect of CO2 enrichment and temperature on wheat production in Sub-humid climate of eastern IGP in India. To address this issue, an Open top chamber (OTCs) experiment was conducted...
Department of Oceanography, University of Cape Town, Rondebosch, 7701, South Africa B. R. Loveday & C. J. C. Reason GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstr. 1-3, 24148, Kiel, Germany W.-C. Dullo University of Edinburgh, Grant Institute, The King's Buildings, Wes...
Subsamples were drilled at a distance of 1 mm for the years 1995–1920 and 2 mm for the older part of the core; the drilling depth was 3 mm using a 0.5 mm dental drill at 1000 rpm. The 1 or 2 mm sample spacing provides approximately monthly or bimonthly resolution, respectively. ...
Reproducible climate reconstructions of the Common Era (1 CE to present) are key to placing industrial-era warming into the context of natural climatic variability. Here we present a community-sourced database of temperature-sensitive proxy records from