Variation of Ice Nucleating Particles in the European Arctic Over the Last Centuries

被引:42
作者
Hartmann, M. [1 ]
Blunier, T. [2 ]
Bruegger, S. O. [3 ,4 ]
Schmale, J. [5 ]
Schwikowski, M. [4 ,6 ]
Vogel, A. [6 ,7 ]
Wex, H. [1 ]
Stratmann, F. [1 ]
机构
[1] Leibniz Inst Tropospher Res, Leipzig, Germany
[2] Univ Copenhagen, Niels Bohr Inst, Ctr Ice & Climate, Copenhagen, Denmark
[3] Univ Bern, Inst Plant Sci, Bern, Switzerland
[4] Univ Bern, Oeschger Ctr Climate Change Res, Bern, Switzerland
[5] Paul Scherrer Inst, Lab Atmospher Chem, Villigen, Switzerland
[6] Paul Scherrer Inst, Lab Environm Chem, Villigen, Switzerland
[7] Goethe Univ, Inst Atmospher & Environm Sci, Frankfurt, Germany
关键词
Arctic; atmospheric aerosol; ice nucleating particles; ice cores; MIXED-PHASE CLOUD; CLIMATE-CHANGE; CORE RECORD; SEA-ICE; NUCLEI; AEROSOLS; SURFACE; OCEAN; WATER; LOMONOSOVFONNA;
D O I
10.1029/2019GL082311
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The historical development of ice nucleating particle concentrations (N-INP) is still unknown. Here, we present for the first time N-INP from the past 500 years at two Arctic sites derived from ice core samples. The samples originate from the EUROCORE ice core (Summit, Central Greenland) and from the Lomo09 ice core (Lomonosovfonna, Svalbard). No long-term trend is obvious in the measured samples, and the overall range of N-INP is comparable to present-day observations. We observe that the short-term variations in N-INP is larger than the long-term variability, but neither anthropogenic pollution nor volcanic eruptions seem to have influenced N-INP in the measured temperature range. Shape and onset temperature of several INP spectra suggest that INP of biogenic origin contributed to the Arctic INP population throughout the past.
引用
收藏
页码:4007 / 4016
页数:10
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