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DOI | 10.1029/2018GL080899 |
Evaluating the Significance of the Contrail Effect on Diurnal Temperature Range Using the Eyjafjallajokull Eruption-Related Flight Disruption | |
Sandhu, Ajvir S.; Baldini, James U. L. | |
2018-12-16 | |
发表期刊 | GEOPHYSICAL RESEARCH LETTERS |
ISSN | 0094-8276 |
EISSN | 1944-8007 |
出版年 | 2018 |
卷号 | 45期号:23页码:13090-13098 |
文章类型 | Article |
语种 | 英语 |
国家 | England |
英文摘要 | Meteorological data collected during the post-9/11 flight grounding in the United States suggested that the removal of contrails increased diurnal temperature range (DTR), but subsequent research has contested this result. The 2010 Eyjafjallajokull eruption resulted in a 97% flight cancelation rate across the UK, offering another rare opportunity to compare DTR under contrail-free skies against those with contrails. Temperature data from 199 UK meteorological stations indicate that a + 3.4 degrees C DTR anomaly occurred during the grounding interval across the region previously affected by the highest flight densities, substantially larger than the + 1.1 degrees C anomaly previously observed but smaller than other DTR anomalies (up to similar to + 6 degrees C) that were independent of the grounding. Although the observed DTR anomalies are largely attributable to weather system migration, a contribution of up to + 1 degrees C from contrail absence appears reconcilable with both the observed time evolution in DTR during the Eyjafjallajokull grounding period and previous results. Plain Language Summary Due to permanent and near-constant aviation activity, directly comparing atmospheric conditions underneath skies with and without contrails under equivalent ambient conditions is difficult. Previous research used the post-9/11 flight groundings in 2001 to detect a contrail effect on diurnal temperature range across the United States. The removal of contrails was found to have increased daytime high temperatures and decreased nighttime low temperatures. However, subsequent research challenged this result and the overall effect of contrails on weather remains unclear. Here we use a very high density network of meteorological stations across the United Kingdom to assess the importance of contrails on diurnal temperature range during a more recent flight grounding following the Eyjafjallajokull volcanic eruption of 2010. We find that subtle, but substantial, temperature shifts related to contrails may have been overprinted by larger shifts in weather systems passing over the United Kingdom. |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000454296600049 |
WOS关键词 | UNITED-STATES ; CLIMATE ; CIRRUS ; IMPACT ; WEATHER ; CLOUDS ; CLEAR |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/28477 |
专题 | 气候变化 |
作者单位 | Univ Durham, Dept Earth Sci, Sci Labs, Durham, England |
推荐引用方式 GB/T 7714 | Sandhu, Ajvir S.,Baldini, James U. L.. Evaluating the Significance of the Contrail Effect on Diurnal Temperature Range Using the Eyjafjallajokull Eruption-Related Flight Disruption[J]. GEOPHYSICAL RESEARCH LETTERS,2018,45(23):13090-13098. |
APA | Sandhu, Ajvir S.,&Baldini, James U. L..(2018).Evaluating the Significance of the Contrail Effect on Diurnal Temperature Range Using the Eyjafjallajokull Eruption-Related Flight Disruption.GEOPHYSICAL RESEARCH LETTERS,45(23),13090-13098. |
MLA | Sandhu, Ajvir S.,et al."Evaluating the Significance of the Contrail Effect on Diurnal Temperature Range Using the Eyjafjallajokull Eruption-Related Flight Disruption".GEOPHYSICAL RESEARCH LETTERS 45.23(2018):13090-13098. |
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