Environmental Role of Rime Chemistry at Selected Mountain Sites in Poland
The results of field experiments on fog pollutant deposition enhanced by local mountain climate, completed by the dendrochronological analysis of the forest response, are presented in this paper. In spite of their low absolute altitude (1,000–1,600 m a.s.l), the Sudetes and the Silesian Beskid form...
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| Published in: | Pure and applied geophysics Vol. 169; no. 5-6; pp. 1093 - 1106 |
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01-05-2012
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| Abstract | The results of field experiments on fog pollutant deposition enhanced by local mountain climate, completed by the dendrochronological analysis of the forest response, are presented in this paper. In spite of their low absolute altitude (1,000–1,600 m a.s.l), the Sudetes and the Silesian Beskid form a noticeable orographic barrier for the airflow of the humid Atlantic air masses. This results in the increase of cloudiness and fog frequency as well as both atmospheric precipitation and horizontal precipitation volume. Between January and December 2009 the daily samples of atmospheric precipitation and rime were collected on three selected mountain tops of similar height. The selected measurement sites were situated along a 300 km WNW-ESE profile parallel to the direction of the prevailing atmospheric circulation. High day-to-day variability of rime water volume, the total ionic content and chemical composition of the individual samples were typical of each measurement site and depended on the emission patterns, synoptic situation and the local climatic conditions influenced chiefly by terrain relief. Significantly larger rime efficiency and pollution deposition via fog were observed at the westernmost Szrenica Mt site rather than more to the southeast at Śnieżnik Mt and Skrzyczne Mt. This difference should be explained by more intense orographic deformation of predominant airflow from the western sector as well as the higher liquid water content of fog in the vicinity of Szrenica. Both temporal and spatial variability of fog deposition correlates closely with the health status of the drilled trees of Norway Spruce (
Picea Abies
) in the Śnieżnik Massif. The averaged annual tree rings width near the local tree line (1,350 m a.s.l.) on the summit dome of Śnieżnik decreased by 71% between 1950 and the early 1980s. This is also the area of the highest rate of atmospheric pollutant deposition due to particularly important role of fog. At an altitude of 1,200 m a.s.l. The relevant changes of ring width were different depending on slope aspect: 60% on western slopes well exposed for orographic fog formation and 42% on eastern slopes where fog deposition is less intense. The results of the dendrochronological analysis provide the evidence for the upward trend of tree rings width since 1981–1984 break through up to date, which should be attributed to the progressive reduction of pollutant emission in Central Europe. |
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| AbstractList | The results of field experiments on fog pollutant deposition enhanced by local mountain climate, completed by the dendrochronological analysis of the forest response, are presented in this paper. In spite of their low absolute altitude (1,000-1,600 m a.s.l), the Sudetes and the Silesian Beskid form a noticeable orographic barrier for the airflow of the humid Atlantic air masses. This results in the increase of cloudiness and fog frequency as well as both atmospheric precipitation and horizontal precipitation volume. Between January and December 2009 the daily samples of atmospheric precipitation and rime were collected on three selected mountain tops of similar height. The selected measurement sites were situated along a 300 km WNW-ESE profile parallel to the direction of the prevailing atmospheric circulation. High day-to-day variability of rime water volume, the total ionic content and chemical composition of the individual samples were typical of each measurement site and depended on the emission patterns, synoptic situation and the local climatic conditions influenced chiefly by terrain relief. Significantly larger rime efficiency and pollution deposition via fog were observed at the westernmost Szrenica Mt site rather than more to the southeast at nienik Mt and Skrzyczne Mt. This difference should be explained by more intense orographic deformation of predominant airflow from the western sector as well as the higher liquid water content of fog in the vicinity of Szrenica. Both temporal and spatial variability of fog deposition correlates closely with the health status of the drilled trees of Norway Spruce (Picea Abies) in the nienik Massif. The averaged annual tree rings width near the local tree line (1,350 m a.s.l.) on the summit dome of nienik decreased by 71% between 1950 and the early 1980s. This is also the area of the highest rate of atmospheric pollutant deposition due to particularly important role of fog. At an altitude of 1,200 m a.s.l. The relevant changes of ring width were different depending on slope aspect: 60% on western slopes well exposed for orographic fog formation and 42% on eastern slopes where fog deposition is less intense. The results of the dendrochronological analysis provide the evidence for the upward trend of tree rings width since 1981-1984 break through up to date, which should be attributed to the progressive reduction of pollutant emission in Central Europe. The results of field experiments on fog pollutant deposition enhanced by local mountain climate, completed by the dendrochronological analysis of the forest response, are presented in this paper. In spite of their low absolute altitude (1,000–1,600 m a.s.l), the Sudetes and the Silesian Beskid form a noticeable orographic barrier for the airflow of the humid Atlantic air masses. This results in the increase of cloudiness and fog frequency as well as both atmospheric precipitation and horizontal precipitation volume. Between January and December 2009 the daily samples of atmospheric precipitation and rime were collected on three selected mountain tops of similar height. The selected measurement sites were situated along a 300 km WNW-ESE profile parallel to the direction of the prevailing atmospheric circulation. High day-to-day variability of rime water volume, the total ionic content and chemical composition of the individual samples were typical of each measurement site and depended on the emission patterns, synoptic situation and the local climatic conditions influenced chiefly by terrain relief. Significantly larger rime efficiency and pollution deposition via fog were observed at the westernmost Szrenica Mt site rather than more to the southeast at Śnieżnik Mt and Skrzyczne Mt. This difference should be explained by more intense orographic deformation of predominant airflow from the western sector as well as the higher liquid water content of fog in the vicinity of Szrenica. Both temporal and spatial variability of fog deposition correlates closely with the health status of the drilled trees of Norway Spruce ( Picea Abies ) in the Śnieżnik Massif. The averaged annual tree rings width near the local tree line (1,350 m a.s.l.) on the summit dome of Śnieżnik decreased by 71% between 1950 and the early 1980s. This is also the area of the highest rate of atmospheric pollutant deposition due to particularly important role of fog. At an altitude of 1,200 m a.s.l. The relevant changes of ring width were different depending on slope aspect: 60% on western slopes well exposed for orographic fog formation and 42% on eastern slopes where fog deposition is less intense. The results of the dendrochronological analysis provide the evidence for the upward trend of tree rings width since 1981–1984 break through up to date, which should be attributed to the progressive reduction of pollutant emission in Central Europe. Issue Title: Special Issue: Fog and Dew Observations and Modeling The results of field experiments on fog pollutant deposition enhanced by local mountain climate, completed by the dendrochronological analysis of the forest response, are presented in this paper. In spite of their low absolute altitude (1,000-1,600 m a.s.l), the Sudetes and the Silesian Beskid form a noticeable orographic barrier for the airflow of the humid Atlantic air masses. This results in the increase of cloudiness and fog frequency as well as both atmospheric precipitation and horizontal precipitation volume. Between January and December 2009 the daily samples of atmospheric precipitation and rime were collected on three selected mountain tops of similar height. The selected measurement sites were situated along a 300 km WNW-ESE profile parallel to the direction of the prevailing atmospheric circulation. High day-to-day variability of rime water volume, the total ionic content and chemical composition of the individual samples were typical of each measurement site and depended on the emission patterns, synoptic situation and the local climatic conditions influenced chiefly by terrain relief. Significantly larger rime efficiency and pollution deposition via fog were observed at the westernmost Szrenica Mt site rather than more to the southeast at nienik Mt and Skrzyczne Mt. This difference should be explained by more intense orographic deformation of predominant airflow from the western sector as well as the higher liquid water content of fog in the vicinity of Szrenica. Both temporal and spatial variability of fog deposition correlates closely with the health status of the drilled trees of Norway Spruce (Picea Abies) in the nienik Massif. The averaged annual tree rings width near the local tree line (1,350 m a.s.l.) on the summit dome of nienik decreased by 71% between 1950 and the early 1980s. This is also the area of the highest rate of atmospheric pollutant deposition due to particularly important role of fog. At an altitude of 1,200 m a.s.l. The relevant changes of ring width were different depending on slope aspect: 60% on western slopes well exposed for orographic fog formation and 42% on eastern slopes where fog deposition is less intense. The results of the dendrochronological analysis provide the evidence for the upward trend of tree rings width since 1981-1984 break through up to date, which should be attributed to the progressive reduction of pollutant emission in Central Europe.[PUBLICATION ABSTRACT] |
| Author | Błaś, Marek Namieśnik, Jacek Polkowska, Żaneta Godek, Michał Cichała-Kamrowska, Katarzyna Sobik, Mieczysław |
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| CitedBy_id | crossref_primary_10_1016_j_scitotenv_2023_161697 crossref_primary_10_1007_s10342_018_01160_4 crossref_primary_10_1080_02723646_2018_1547872 crossref_primary_10_1371_journal_pone_0165967 crossref_primary_10_1016_j_atmosenv_2021_118877 crossref_primary_10_3390_f10110943 crossref_primary_10_2478_ffp_2020_0018 crossref_primary_10_1016_j_foreco_2018_12_052 |
| Cites_doi | 10.1016/j.envsci.2006.05.002 10.1007/978-94-009-4003-1_11 10.1007/978-3-642-76995-5 10.3402/tellusb.v44i1.15421 10.1023/A:1013867620159 |
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| Keywords | mountain climate Air pollution rime spruce dendrochronology fog deposition total ionic content experimental studies altitude mountains terrains air upper Quaternary pollution variability trees frequency Pinaceae Upper Carboniferous water content deformation relief Cenozoic Picea direction efficiency atmospheric precipitation gymnosperms Quaternary Plantae Carboniferous climate forests pollutants Paleozoic Silesian Abies upper Paleozoic Coniferales Spermatophyta Phanerozoic atmospheric circulation Holocene Atlantic chemical composition tree rings |
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| Snippet | The results of field experiments on fog pollutant deposition enhanced by local mountain climate, completed by the dendrochronological analysis of the forest... Issue Title: Special Issue: Fog and Dew Observations and Modeling The results of field experiments on fog pollutant deposition enhanced by local mountain... |
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| SubjectTerms | Air flow Air masses Air pollution Altitude Applied geophysics Atmospheric circulation Atmospheric pollution deposition Chemistry Climatic conditions Earth and Environmental Science Earth Sciences Earth, ocean, space Emission measurements Engineering and environment geology. Geothermics Exact sciences and technology Field tests Fog Geophysics/Geodesy Humidity Internal geophysics Mountains Picea abies Pine trees Pollutant deposition Pollution control Pollution, environment geology Precipitation Rime Water content |
| Title | Environmental Role of Rime Chemistry at Selected Mountain Sites in Poland |
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