Ocean salinities reveal strong global water cycle intensification during 1950 to 2000.
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Metrological challenges for measurements of key climatological observables: Oceanic salinity and pH, and atmospheric humidity. Part 1: OverviewGlobal water cycle amplifying at less than the Clausius-Clapeyron rateOverlooked possibility of a collapsed Atlantic Meridional Overturning Circulation in warming climateMetrological challenges for measurements of key climatological observables, Part 4: Atmospheric relative humidityPronounced zonal heterogeneity in Eocene southern high-latitude sea surface temperaturesInfectious disease emergence and global change: thinking systemically in a shrinking worldIdentifying external influences on global precipitationAvian community responses to variability in river hydrologyAn observing system simulation for Southern Ocean carbon dioxide uptake.Genome of the halotolerant green alga Picochlorum sp. reveals strategies for thriving under fluctuating environmental conditions.Timing of the departure of ocean biogeochemical cycles from the preindustrial state.Characterizing differences in precipitation regimes of extreme wet and dry years: implications for climate change experiments.Assessment of future changes in water availability and aridity.Sea-ice transport driving Southern Ocean salinity and its recent trends.Separating decadal global water cycle variability from sea level rise.Terrestrial water fluxes dominated by transpiration.Climate-driven polar motion: 2003-2015.Sensitivity of grassland plant community composition to spatial vs. temporal variation in precipitation.Importance of long-term cycles for predicting water level dynamics in natural lakes.Mapping the salinity gradient in a microfluidic device with schlieren imaging.Decadal trends of the upper ocean salinity in the tropical Indo-Pacific since mid-1990sInterpreting beta-diversity components over time to conserve metacommunities in highly dynamic ecosystems.North Atlantic salinity as a predictor of Sahel rainfall.Global warming-induced upper-ocean freshening and the intensification of super typhoonsEthylene--and oxygen signalling--drive plant survival during flooding.Membrane transporters mediating root signalling and adaptive responses to oxygen deprivation and soil flooding.Abrupt cooling over the North Atlantic in modern climate models.The dominant role of climate change in determining changes in evapotranspiration in Xinjiang, China from 2001 to 2012Scientifically literate action: key barriers and facilitators across context and content.Sea surface temperature and salinity from French research vessels, 2001-2013.Cirrus cloud seeding: a climate engineering mechanism with reduced side effects?High salinity conveys thermotolerance in the coral model Aiptasia.Environmental proteomics of the mussel Mytilus: implications for tolerance to stress and change in limits of biogeographic ranges in response to climate change.Long-term increases in tropical flowering activity across growth forms in response to rising CO2 and climate change.Negative soil moisture-precipitation feedback in dry and wet regions.Critical impact of vegetation physiology on the continental hydrologic cycle in response to increasing CO2.Changes in benthic ecosystems and ocean circulation in the Southeast Atlantic across Eocene Thermal Maximum 2Wetland monitoring with Global Navigation Satellite System reflectometry.Homeostasis of Second Messenger Cyclic-di-AMP Is Critical for Cyanobacterial Fitness and Acclimation to Abiotic Stress.Water Vapor Transfer and Near-Surface Salinity Contrasts in the North Atlantic Ocean.
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Ocean salinities reveal strong global water cycle intensification during 1950 to 2000.
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2012 nî lūn-bûn
@nan
2012 թուականի Ապրիլին հրատարակուած գիտական յօդուած
@hyw
2012 թվականի ապրիլին հրատարակված գիտական հոդված
@hy
2012年の論文
@ja
2012年論文
@yue
2012年論文
@zh-hant
2012年論文
@zh-hk
2012年論文
@zh-mo
2012年論文
@zh-tw
2012年论文
@wuu
name
Ocean salinities reveal strong global water cycle intensification during 1950 to 2000.
@ast
Ocean salinities reveal strong global water cycle intensification during 1950 to 2000.
@en
Ocean salinities reveal strong global water cycle intensification during 1950 to 2000.
@nl
type
label
Ocean salinities reveal strong global water cycle intensification during 1950 to 2000.
@ast
Ocean salinities reveal strong global water cycle intensification during 1950 to 2000.
@en
Ocean salinities reveal strong global water cycle intensification during 1950 to 2000.
@nl
prefLabel
Ocean salinities reveal strong global water cycle intensification during 1950 to 2000.
@ast
Ocean salinities reveal strong global water cycle intensification during 1950 to 2000.
@en
Ocean salinities reveal strong global water cycle intensification during 1950 to 2000.
@nl
P2860
P356
P1433
P1476
Ocean salinities reveal strong global water cycle intensification during 1950 to 2000.
@en
P2093
Susan E Wijffels
P2860
P304
P356
10.1126/SCIENCE.1212222
P407
P577
2012-04-01T00:00:00Z