Advances in Earth Science ›› 2024, Vol. 39 ›› Issue (11): 1112-1122.DOI: 10.11867/j.issn.1001-8166.2024.083
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Yaohui LI1(), Siqi HE1,2(
), Ying XU2,3
Received:
2024-09-21
Revised:
2024-10-21
Online:
2024-11-10
Published:
2024-12-19
Contact:
Siqi HE
About author:
LI Yaohui, research areas include research on weather, climate, climate change and aviation meteorology. E-mail: li-yaohui@163.com
Supported by:
通讯作者:
何思奇
作者简介:
李耀辉,主要从事天气、气候与气候变化以及航空气象等方面的研究. E-mail:li-yaohui@163.com
基金资助:
CLC Number:
Yaohui LI, Siqi HE, Ying XU. Progress of Research on Aviation and Climate Warming[J]. Advances in Earth Science, 2024, 39(11): 1112-1122.
李耀辉, 何思奇, 徐影. 航空与气候变暖研究进展[J]. 地球科学进展, 2024, 39(11): 1112-1122.
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URL: http://www.adearth.ac.cn/EN/10.11867/j.issn.1001-8166.2024.083
Fig. 1 Best assessment of climate forcing for different types of emissions from commercial aviation between 1940 and 2018The ERF takes into account short-term feedbacks in the climate system that are not accounted for in traditional Radiative Forcing (RF) assessments, best estimates outside parentheses, confidence intervals in parentheses (modified after reference [10])
Fig. 2 Radiative forcing of the aviation componentContrail and CO2 estimates represent 2011 emission levels (modified after reference [39])① https://www.reading.ac.uk/news/2024/Expert-Comment/Turbulence-is-apparent-cause-of-flight-death② https://www.weforum.org/agenda/2024/08/turbulence-climate-change/③ https://www.canada.ca/en/transportation-safety-board/news/2017/02/tsb_reminds_aircraftpassengerstobuckleupafter21peopleinjuredduri.html④ https://graphics.thomsonreuters.com/testfiles/2024/nZfKwwIgUlKA/
Fig. 3 Time series of 250 hPa annual mean wind characteristics in the North Atlantic for the period 1979-2017 (modified after reference [55])(a) Vertical shear of latitudinal winds; (b) Latitudinal wind speed
Fig. 4 Histogram of journey times between New York’s JFK and London’s Heathrow airportsHistograms showing the probability distribution of daily (a) eastbound and (b) westbound shortest route durations at 200 hPa altitude. The width of the interval used to calculate the probabilities is 1 min. The paths are calculated for 20 consecutive winters (from 1 December to 28 February) using the pre-industrial control simulation of the GFDL CM2.1 climate model and a double CO? concentration simulation. The solid black line is fitted to a normal distribution; the dashed black line indicates the duration of the great circle route in still air (modified after reference [21])
Fig. 5 Mean latitude of rapids in the western and eastern Atlantic for five different climate modelsFor each pair of points, the mean (symbols) and standard deviation (solid line) of the current climate are on the left, and the mean of the climate and its standard deviation for the future (2073-2099) high GHG emission scenario are on the right. For comparison, the mean latitude of rapids in the western (dotted line) and eastern Atlantic (dashed line) of the ERA Interim reanalysis data for the period 1979-2005 is indicated (modified after reference [20])
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