Results 51 to 60 of about 736 (153)
Ocean Nd-144 from an isotope enabled coarse resolution (3˚), ocean-only simulation run from the LGM (22ka) to present day using iPOP2. Reprocessed original netcdf3 file to netcdf4 using Xarray
Alexandra Jahn (8148714)
core +1 more source
Ocean temperature from an isotope enabled coarse resolution (3˚), ocean-only simulation run from the LGM (22ka) to present day using iPOP2. Reprocessed original netcdf3 file to netcdf4 using Xarray
Alexandra Jahn (8148714)
core +1 more source
Background To assess the precision and agreement of measurements of higher order aberrations (HOAs) obtained with a ray tracing aberrometer (iTrace) and a Hartmann-Shack aberrometer (Topcon KR-1 W).
Zequan Xu +4 more
doaj +1 more source
Abstract The relationship between changes in surface air temperature and sea surface temperature is important for understanding past and future climate change. In this study, we use reconstructions and model simulations to investigate the ratio of global mean air versus sea surface temperature change (S) during the Last Glacial Maximum (LGM).
Chenyu Zhu, Yahui Jin
wiley +1 more source
Ideal age as an ocean tracer from an isotope enabled coarse resolution (3˚), ocean-only simulation run from the LGM (22ka) to present day using iPOP2. Reprocessed original netcdf3 file to netcdf4 using Xarray
Alexandra Jahn (8148714)
core +1 more source
Revisiting Western United States Hydroclimate During the Last Deglaciation
During the last ice age, the western United States was covered by large lakes, sustained partly by higher levels of precipitation. Increased rainfall was driven by the atmospheric circulation associated with the presence of large North American ice ...
Minmin Fu
doaj +1 more source
A Brief Note on Supercooled Glacial Deep Waters
Abstract According to hydrographic profiles, approximately 2%–5% of the present‐day deep Southern Ocean contains supercooled waters that are below the freezing point. Which role these supercooled waters may have played under glacial conditions is an open question.
Miho Ishizu +2 more
wiley +1 more source
Ocean Nd-143 from an isotope enabled coarse resolution (3˚), ocean-only simulation run from the LGM (22ka) to present day using iPOP2. Reprocessed original netcdf3 file to netcdf4 using Xarray
Alexandra Jahn (8148714)
core +1 more source
Minimal AMOC Impact in Alaska During the Younger Dryas
Abstract The Younger Dryas chronozone (YD), between ∼12,900 and 11,600 years ago, represents a climatically dynamic period in Earth's history that was defined by rapid millennial‐scale climate changes. The cause of the climate change during the YD is typically attributed to substantial meltwater flux into the North Atlantic, which weakened the Atlantic
Paul S. Wilcox, Minmin Fu
wiley +1 more source
ABSTRACT Future projections of climate change in the subtropics suggest warming and drying, while evidence from warm periods in the past shows increases in subtropical temperatures and precipitation. Eastern Australia is subject to interannual hydroclimate drivers and has experienced extreme flooding and droughts in recent years.
Joan Macalalad +5 more
wiley +1 more source

