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[PDF] Top 20 What controls the isotopic composition of Greenland surface snow?

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What controls the isotopic composition of Greenland surface snow?

What controls the isotopic composition of Greenland surface snow?

... CROCUS surface–atmosphere mass flux and our isotopic ...the surface reveal earlier precipitation and snow surface isotope values similar to a tape recorder played in ...of ... See full document

16

ISOTOPIC COMPOSITION OF PRECIPITATION IN A TOPOGRAPHICALLY COMPLEX, SEASONALLY SNOW-DOMINATED WATERSHED: HYDROMETEOROLOGICAL CONTROLS AND VARIATIONS FROM THE GLOBAL METEORIC WATER LINE

ISOTOPIC COMPOSITION OF PRECIPITATION IN A TOPOGRAPHICALLY COMPLEX, SEASONALLY SNOW-DOMINATED WATERSHED: HYDROMETEOROLOGICAL CONTROLS AND VARIATIONS FROM THE GLOBAL METEORIC WATER LINE

... spatial controls on the isotopic composition of precipitation in mid-continent watersheds where multiple factors control the isotopic composition of meteoric ...these controls on ... See full document

94

Controls on the Sulfur Isotopic Composition of Carbonate-Associated Sulfate

Controls on the Sulfur Isotopic Composition of Carbonate-Associated Sulfate

... the surface of the water body or a marginal environment, after which the brine may have flowed down slope and displaced fresher overlying water, or gypsum crystals may have been transported by mass flow or dropped ... See full document

262

Evaporation Depth Controls the Relationship Between Soil Water Mobility and Soil Water Isotopic Composition

Evaporation Depth Controls the Relationship Between Soil Water Mobility and Soil Water Isotopic Composition

... water composition in a sandy soil but failed to do so in silty and clayey soils, including a loamy ...the isotopic composition of spiked water in sandy ... See full document

169

Towards a tracer based conceptualization of meltwater dynamics and streamflow response in a glacierized catchment

Towards a tracer based conceptualization of meltwater dynamics and streamflow response in a glacierized catchment

... the controls on the spatial and temporal patterns of the tracer signature in the main stream, its selected tributaries, shallow groundwater, snowmelt and glacier melt over a 3- year ...and isotopic ... See full document

19

Acquisition of isotopic composition for surface snow in East Antarctica and the links to climatic parameters

Acquisition of isotopic composition for surface snow in East Antarctica and the links to climatic parameters

... Water isotopic composition of shallow and deep ice cores has long been used for reconstructing past climatic conditions in polar regions (Jouzel et ...water isotopic composition (δ 18 O or δD) ... See full document

16

Experimental observation of transient 18 O interaction between snow and advective airflow under various temperature gradient conditions

Experimental observation of transient 18 O interaction between snow and advective airflow under various temperature gradient conditions

... and Greenland snow profile, strong interactions between the atmosphere and snow oc- cur, especially in the first 2 m (Neumann and Waddington, 2004; Town et ...between snow and the atmospheric ... See full document

11

Evaluation of lacustrine groundwater discharge, hydrologic partitioning, and nutrient budgets in a proglacial lake in the Qinghai–Tibet Plateau: using 222Rn and stable isotopes

Evaluation of lacustrine groundwater discharge, hydrologic partitioning, and nutrient budgets in a proglacial lake in the Qinghai–Tibet Plateau: using 222Rn and stable isotopes

... The isotopic compositions of the lake water and porewa- ter are significantly isotopically depleted, with values close to the compositions of glaciers and surface snow in the QTP, suggesting the lake ... See full document

20

Non-climatic signal in ice core records: lessons from Antarctic megadunes

Non-climatic signal in ice core records: lessons from Antarctic megadunes

... 2013–2015). Snow accumulation rate and isotope content (δD, δ 18 O and δ 17 O) were measured along the 2 km pro- file across the megadune ridge accompanied by precise GPS altitude measurements and ground ... See full document

11

Archival processes of the water stable isotope signal in East Antarctic ice cores

Archival processes of the water stable isotope signal in East Antarctic ice cores

... the snow isotopic composition can- not be neglected at the atmosphere–snow interface (Town et ...and isotopic composition of surface snow is different from the one ... See full document

22

Neither dust nor black carbon causing apparent albedo decline in Greenland's dry snow zone: Implications for MODIS C5 surface reflectance

Neither dust nor black carbon causing apparent albedo decline in Greenland's dry snow zone: Implications for MODIS C5 surface reflectance

... dry snow zone using C5 MODIS data sets (Figure ...dry snow albedo changes and utilize only the best available data (see methods, supporting information Text ...MCD43A3 surface re fl ectance product ... See full document

11

Simulating ice core 10 Be on the glacial–interglacial timescale

Simulating ice core 10 Be on the glacial–interglacial timescale

... In recent years, several studies improved the knowledge on processes which influence atmospheric 10 Be in polar regions. Atmospheric production rates have been calculated within elaborative Monte Carlo simulations of ... See full document

19

Assessing land–ocean connectivity via submarine groundwater discharge (SGD)
in the Ria Formosa Lagoon (Portugal): combining radon measurements and
stable isotope hydrology

Assessing land–ocean connectivity via submarine groundwater discharge (SGD) in the Ria Formosa Lagoon (Portugal): combining radon measurements and stable isotope hydrology

... Indeed, as noted by Beck et al. (2007), SGD-borne chem- ical load into coastal systems is usually predicted by com- bining measurements of source composition with SGD esti- mates. Linking these two data sets ... See full document

22

Simulating ice core 10Be on the glacial–interglacial timescale

Simulating ice core 10Be on the glacial–interglacial timescale

... for Greenland and Antarctica, respec- ...the Greenland results surprisingly ...on Greenland model results and use an over- all dry deposition velocity of ...−3 snow ] for Greenland ... See full document

21

Nitrate deposition to surface snow at Summit, Greenland, following the 9 November 2000 solar proton event

Nitrate deposition to surface snow at Summit, Greenland, following the 9 November 2000 solar proton event

... directly over Summit both with and without SPEs. The method of calculating modeled wet deposition instantaneously from the entire atmospheric column is useful for determining the maximum potential deposition of nitrate ... See full document

22

Determination of Isotopic Composition and Concentration of Uranium and Boron by Thermal Ionization Mass Spectrometric Isotopic Dilution Technique

Determination of Isotopic Composition and Concentration of Uranium and Boron by Thermal Ionization Mass Spectrometric Isotopic Dilution Technique

... of isotopic dilution technique, a series of boron mixtures were prepared by mixing a known aliquot of spike solution (3151 ppm boron) with certain portion of freshly prepared standard solution (3400 ppm boron) ... See full document

6

Air-snow exchange of HNO3 and NOy at Summit, Greenland

Air-snow exchange of HNO3 and NOy at Summit, Greenland

... We presentedone case study where the NO 3- inventory in snow are ordersof magnitudesmaller than would be expectedfrom theNOyfluxes.However, thefactthatNO3- inventories were increasedtoo [r] ... See full document

13

The growth of sublimation crystals and surface hoar on the Antarctic plateau

The growth of sublimation crystals and surface hoar on the Antarctic plateau

... were surface hoar crystals, which very commonly grow on any snow surface that cools radiatively in the absence of strong winds (Cabanes et ...2002). Surface hoar crystals are formed by the ... See full document

11

The Late Quaternary Paleolimnology of Lake Ontario

The Late Quaternary Paleolimnology of Lake Ontario

... particular, it has been suggested that meltwater from the ablating Laurentide Ice Sheet (LIS) was routed through the Great Lakes to the Atlantic Ocean, weakening thermohaline circulation (THC) in the Atlantic Meridional ... See full document

266

Use of satellite derived data for characterization of snow cover and simulation of snowmelt runoff through a distributed physically based model of runoff generation

Use of satellite derived data for characterization of snow cover and simulation of snowmelt runoff through a distributed physically based model of runoff generation

... the snow spatial distribution and temporal variability consists in cou- pling satellite snow cover products with ground-based mete- orological measurements and snow pack ...of snow covered ... See full document

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