RECORDS of sulphate and nitrate concentrations in ice cores show that these concentrations have increased recently because of the long-range transport of pollution from middle latitudes1–5. But these records have been neither complete enough nor long enough to allow an assessment of their sensitivity to variations in the emissions of sulphate and nitrate precursors. We have now analysed sections from an ice core in South Greenland which have allowed us to extend its sulphate and nitrate record back from 1869 to 1767. This longer record has enabled us to determine the pre-industrial natural interannual variability of non-sea-salt sulphate and nitrate. We find that the background concentration in the remote atmosphere over South Greenland is ...
This work represents an analysis of the spatial and temporal variability of nitrate deposition and p...
pH is a master variable that controls many chemical reactions in nature due to the abundance of acid...
Reconstruction of past changes in Arctic sea ice extent may be critical for understanding its future...
An ice core in south Greenland covering the period 1869 to 1984 was analyzed for oxygen isotopes and...
An understanding of the phenomenon of acid rain requires the identification of the sources of the sp...
210-year records of dust concentration, electrical conductivity, acidity (pH), non-sea salt sulfate ...
An understanding of the phenomenon of acid rain requires the identification of the sources of the sp...
Comparison of ice-core nss sulfate records (two sites in Greenland and one in the North Pacific) wit...
High-resolution snow chemistry records have been recovered from a site close to the South Pole, cove...
The spatial, temporal, source and physical controls on chloride, nitrate, sulfate and sodium in sout...
Methanesulfonate (MSA) in ice cores has attracted attention as a possible tracer of past oceanic emi...
International audienceSulfur isotopes of sulfate have been measured in a discontinuous set of polar ...
The concentration of methanesulfonic acid (MSA) was determined in a shallow south central Greenland ...
The Southeastern Greenland Dome (SE-Dome) has both a high elevation and a high accumulation rate (1....
Nitrate records from six Greenland ice cores covering the period 1789 to 1995 show a significant cor...
This work represents an analysis of the spatial and temporal variability of nitrate deposition and p...
pH is a master variable that controls many chemical reactions in nature due to the abundance of acid...
Reconstruction of past changes in Arctic sea ice extent may be critical for understanding its future...
An ice core in south Greenland covering the period 1869 to 1984 was analyzed for oxygen isotopes and...
An understanding of the phenomenon of acid rain requires the identification of the sources of the sp...
210-year records of dust concentration, electrical conductivity, acidity (pH), non-sea salt sulfate ...
An understanding of the phenomenon of acid rain requires the identification of the sources of the sp...
Comparison of ice-core nss sulfate records (two sites in Greenland and one in the North Pacific) wit...
High-resolution snow chemistry records have been recovered from a site close to the South Pole, cove...
The spatial, temporal, source and physical controls on chloride, nitrate, sulfate and sodium in sout...
Methanesulfonate (MSA) in ice cores has attracted attention as a possible tracer of past oceanic emi...
International audienceSulfur isotopes of sulfate have been measured in a discontinuous set of polar ...
The concentration of methanesulfonic acid (MSA) was determined in a shallow south central Greenland ...
The Southeastern Greenland Dome (SE-Dome) has both a high elevation and a high accumulation rate (1....
Nitrate records from six Greenland ice cores covering the period 1789 to 1995 show a significant cor...
This work represents an analysis of the spatial and temporal variability of nitrate deposition and p...
pH is a master variable that controls many chemical reactions in nature due to the abundance of acid...
Reconstruction of past changes in Arctic sea ice extent may be critical for understanding its future...