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(Table 4) Results of the transport-reaction modelling applied to MIC data
This dataset has no description
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Measurements of An Autonomous Flow through Salinity and Temperature Perturbat...
An ex situ experimental mesocosm system was employed to test the effects of climate change drivers temperature, salinity, and reduced light on Arctic kelp communities in... -
Hydrographic parameters, dissolved CH4, atmospheric CH4 and CO2 along the riv...
In August 2020 the research vessel Albis investigated the river Elbe from Schmielka towards Geesthacht. Basic hydrographic parameters were measured continuously, with a portable... -
Gas exchange of Aleppo Pine seedlings including emissions of biogenic volatil...
The data describes plant gas exchange dynamics (CO2, H2O) together with online proton transfer reaction mass spectrometry measurements of biogenic volatile organic compound... -
(Table 1) Horizontal and vertical ice flow velocities for seven markers aroun...
Combined geodetic, geophysical and glaciological in situ measurements are interpreted regarding surface height changes over subglacial Lake Vostok and the local mass balance of... -
(Table T1) Initial porosity, permeability, flow rate and hydraulic conductivi...
Vertical permeability testing was conducted on 10 whole-round core samples collected from Sites 1173 and 1174 from Ocean Drilling Program Leg 190. Constant-flow permeability... -
(Table T1) Summary of permeability testing in sediments of five ODP Leg 201 s...
Constant-flow permeability tests were conducted on core samples from Ocean Drilling Program Leg 201 from the eastern equatorial Pacific and the Peru margin. Eighteen whole-round... -
Age determination and sedimentation rates of ODP Hole 119-740A (Table 1)
Unconsolidated sediments recovered at Site 740 include approximately 23 m of interbedded siliceous ooze and silty clay (pebbly mud), which was tentatively assigned a late... -
Tab. 1: Results of the movement measurements on the blue ice-field Blåisen
In January/February 1985 a German-South African expedition had the opportunity to repeat measurements made by means of stakes planted in 1951 (Norwegian-British-Swedish... -
Interval transmissivities and permeabilities in ODP Hole 129-801C (Table 2)
Bulk permeability was determined from drillstring packer measurements in ODP Hole 801C in Jurassic oceanic crust in the western Pacific. The values average 8 * 10-14 m2 over 93... -
Seawater carbonate chemistry and physiological performance parameters of Carc...
Ocean acidification causes an accumulation of CO2 in marine organisms and leads to shifts in acid-base parameters. Acid-base regulation in gill breathers involves a net increase... -
Seawater carbonate chemistry and calcification rate of crustose coralline alga
Prior exposure to variable environmental conditions is predicted to influence the resilience of marine organisms to global change. We conducted complementary 4-month field and... -
Seawater carbonate chemistry and net calcification, relative electron transpo...
Ocean acidification (OA) and nutrient enrichment threaten the persistence of near shore ecosystems, yet little is known about their combined effects on marine organisms. Here,... -
Seawater carbonate chemistry and net community calcification (NCC) and net co...
There is a long history of examining the impacts of nutrient pollution and pH on coral reefs. However, little is known about how these two stressors interact and influence coral... -
Coral-algae metabolism and diurnal changes in the CO2-carbonate system of bul...
Precise measurements were conducted in continuous flow seawater mesocosms located in full sunlight that compared metabolic response of coral, coral-macroalgae and macroalgae... -
Seawater carbonate chemistry and resource allocation and extracellular acid-b...
Anthropogenic CO2 emission will lead to an increase in seawater pCO2 of up to 80-100 Pa (800-1000 µatm) within this century and to an acidification of the oceans. Green sea... -
(Table A4) Stable hydrogen isotopic composition of n-C27, n-C29 and n-C31 alk...
Standard deviations and n-values are not reported for aerosol dD values because no field replicates were collected. The pooled analytical uncertainty for these samples was 1.8... -
(Table A3) Concentration of n-alkanes per air volume in old-growth forest Web...
Standard deviations and n-values are reported are not reported for aerosol concentrations because no field replicates were collected. -
(Table T4) Flow-through permeability properties of sediments from ODP Leg 205...
This dataset has no description
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Continuous FerryBox measurements along RV POLARSTERN cruise PS122/1
Oceanographic underway data were collected by the FerryBox on board RV POLARSTERN. The system is supplied by a sea water inlet at about 5 meters depth. As part of the MOSAiC...