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Heating induced temperature difference measurements from SIMBA-type sea ice m...
Temperature and heating-induced temperature differences were measured along a chain of thermistors. SIMBA 2012T32 (a.k.a. ronnie_07) is an autonomous instrument that was... -
Heating induced temperature difference measurements from SIMBA-type sea ice m...
Temperature and heating-induced temperature differences were measured along a chain of thermistors. SIMBA 2022T98 (a.k.a. UIT_0301R) is an autonomous instrument that was... -
Bioassays quantifying the adverse effects of three strains of the harmful din...
RTgill-W1 gill cells of the rainbow trout (Oncorhynchus mykiss) were subjected to supernatants from exponentially grown Alexandrium pseudogonyaulax cultures for 24 h to create... -
Bioassays quantifying the adverse effects of three strains of the harmful din...
RTgill-W1 gill cells of the rainbow trout (Oncorhynchus mykiss) were subjected to supernatants from exponentially grown Alexandrium pseudogonyaulax cultures for 24 h to create... -
Bioassays quantifying the adverse effects of purified goniodomins (GDs) on th...
RTgill-W1 gill cells of the rainbow trout (Oncorhynchus mykiss) were subjected to purified goniodomins (GDs) for 24 h to create dose-response curves. The bioassays were carried... -
Bioassays quantifying the adverse effects of purified goniodomins (GDs) on th...
RTgill-W1 gill cells of the rainbow trout (Oncorhynchus mykiss) were subjected to purified goniodomins (GDs) for 24 h to create dose-response curves. The bioassays were carried... -
Frozen fraction of field blind samples from Antarctica, Neumayer Station III,...
Ice nucleating particles (INPs) are important atmospheric particles influencing the formation of ice in clouds. Their sources and atmospheric concentrations currently are... -
Frozen fraction of INP samples from Antarctica, Neumayer Station III, measure...
Ice nucleating particles (INPs) are important atmospheric particles influencing the formation of ice in clouds. Their sources and atmospheric concentrations currently are... -
Ice nucleating particle concentration of samples from Antarctica, Neumayer St...
Ice nucleating particles (INPs) are important atmospheric particles influencing the formation of ice in clouds. Their sources and atmospheric concentrations currently are... -
Frozen fraction of field blind samples from Antarctica, Neumayer Station III,...
Ice nucleating particles (INPs) are important atmospheric particles influencing the formation of ice in clouds. Their sources and atmospheric concentrations currently are... -
Frozen fraction of INP samples from Antarctica, Neumayer Station III, measure...
Ice nucleating particles (INPs) are important atmospheric particles influencing the formation of ice in clouds. Their sources and atmospheric concentrations currently are... -
Ice nucleating particle concentration of samples from Antarctica, Neumayer St...
Ice nucleating particles (INPs) are important atmospheric particles influencing the formation of ice in clouds. Their sources and atmospheric concentrations currently are... -
Frozen fraction of heated INP samples from Antarctica, Neumayer Station III, ...
Ice nucleating particles (INPs) are important atmospheric particles influencing the formation of ice in clouds. Their sources and atmospheric concentrations currently are... -
Ice nucleating particle concentration from which the median value of the resp...
Ice nucleating particles (INPs) are important atmospheric particles influencing the formation of ice in clouds. Their sources and atmospheric concentrations currently are... -
Ice nucleating particle concentration from which the median value of the resp...
Ice nucleating particles (INPs) are important atmospheric particles influencing the formation of ice in clouds. Their sources and atmospheric concentrations currently are... -
Electrical conductivity from IODP Hole 333-C0011C
Geocode = [m CSF-A] Top Core depth (below sea floor) -
Electrical conductivity from IODP Hole 333-C0011D
Geocode = [m CSF-A] Top Core depth (below sea floor) -
Electrical conductivity from IODP Hole 333-C0012C
Geocode = [m CSF-A] Top Core depth (below sea floor) -
Electrical conductivity from IODP Hole 333-C0012D
Geocode = [m CSF-A] Top Core depth (below sea floor) -
Electrical conductivity from IODP Hole 333-C0012E
Geocode = [m CSF-A] Top Core depth (below sea floor)
