Advances in Meteorology

Advances in Meteorology / 2017 / Article
Special Issue

Stratospheric Processes and Their Role in Climate

View this Special Issue

Research Article | Open Access

Volume 2017 |Article ID 8707234 | https://doi.org/10.1155/2017/8707234

Jinglin Zhang, Jian Shang, Guoyu Zhang, "Verification for Different Contrail Parameterizations Based on Integrated Satellite Observation and ECMWF Reanalysis Data", Advances in Meteorology, vol. 2017, Article ID 8707234, 11 pages, 2017. https://doi.org/10.1155/2017/8707234

Verification for Different Contrail Parameterizations Based on Integrated Satellite Observation and ECMWF Reanalysis Data

Academic Editor: Yoshihiro Tomikawa
Received26 May 2017
Revised07 Aug 2017
Accepted22 Aug 2017
Published01 Oct 2017

Abstract

Aviation induced cloud termed contrail plays a more and more important role in the climate change, which makes a significant contribution to anthropogenic climate forcing through impacting the coverage of cirrus in the intersection of troposphere and stratosphere. In this paper, we propose one novel automatic contrail detecting method based on Himawari-8 stationary satellite imagery and two kinds of potential contrail coverage (PCC1 and PCC2) from contrail parameterization in ECHAM4 and HadGEM2. In addition, we propose one new climatological index called contrail occurrence and persistence (COP). According to the algorithm identification (AI) and artificial visual inspection (AVI), COP measured from Himawari-8 stationary satellite imagery is related to upper tropospheric relative humidity over ice (RHI) computed with the ECMWF reanalysis data by simple linear regression. Similarly, we compared the linear correlation between COP and PCCs fractions and found that PCC1 has better correspondence with COP than PCC2.

1. Introduction

The cloud is an important regulator of the energy budget of the earth system and the most significant uncertainty factor in climate change [14]. Contrail is a special kind of cloud, caused by the aircraft engine emissions from the exhaust gas mixed with the surrounding air and the condensation of water vapor. As one kind of condensation trails, contrail is the direct evidence for the impact of air traffic on cloud cover. The ambient relative humidity is close to saturation, and the atmospheric state is relatively stable to produce contrail. In general, the formation of cirrus requires temperature below −40°C and relative humidity of 145%–165% or more in the stable atmospheric state [5], while the contrail can persist in weakly saturated condition (relative humidity 100%–110%). Compared to the natural cirrus, the contrails are more likely to occur and persist at the upper troposphere and lower stratosphere, which affect the coverage of the high-level cirrus. Similar to natural cirrus clouds, it consists of tiny ice particles and interacts with the radiation field, which has a net warming effect on the earth-atmosphere system [68]. According to the recent study [9], aircraft induced contrails contribute more than the CO2 caused by the airplane flight to global warming. Thus, one considerate detection framework will help researchers to understand the influence of contrails in climate change better. Generally, contrails are divided into three types: young, mature, and old in terms of contrail width and shape. A young contrail was defined as a linear shape with approximately a width less than 3 km and a maximum distance less than 200 km. The mature contrail maintains a linear shape with an approximate width less than 7 km. The old contrail gradually loses the linear shape and develops into the contrail cirrus. It can be observed that a mature contrail has larger brightness temperature difference (BTD) values than old contrails.

For the human visual verification, it is easy to identify linear structures from both ground-based and satellite images as shown in Figure 1. Thus, early explorations about contrail detection mainly exploit the visual examination to detect contrails in satellite images. For example, Degrand et al. (1990) applied hardcopy displays of high-resolution Defense Meteorological Satellite Program data to identify contrails. Degrand et al. (1991) manually interpreted contrails on satellite images over North America and in particular over the United States. Travis (1996) manually counted pixels to determine the width and length of the contrails. All of these manual inspection methods are highly subjective and very time-consuming.

In order to overcome the limitations of manual detection methods for contrails, researchers attempted to develop automatic algorithms to detect contrails depending on satellite imagery. Mannstein et al. (1999) introduced a contrail detection algorithm (CDA) to recognize linear-shaped contrails on satellite images, which is operated on the brightness temperature difference between the 10.8 μm and 12 μm channels. Recently, other studies incorporated CDA to detect contrails. Palikonda et al. (2001) identified the contrails over the United States in AVHRR and MODIS images with CDA method. More recently, Hetzheim [10] proposed a very complicated approach using mathematical methods to detect contrails based on texture or stochastic behaviors of contrails. Although these mathematical methods may distinguish contrails well from background of the satellite images, they are very time-consuming.

To the best of our knowledge, there are still some open questions concerning contrail occurrence, persistence, and spreading, which cause uncertainties in the contrail detection. New generation meteorological satellite like Himawari-8 with 16 multispectral channels captures high quality satellite imagery. Meanwhile stationary satellite imagery with both high spatial and temporal resolution are necessary to locate the linear contrails and track the process from linear contrail (occurrence) to contrail cirrus (persistence), in order to resolve the problem of contrail cirrus overlap and limitation of polar satellite overpass time relative to traffic diurnal cycle. With automatic contrail detection methods, previous research works [1113] mainly focused on heavily flown regions like the North Atlantic flight corridor and Europe regions to compute the contrail coverage and related radiative forcing impact. Little study about contrail was carried out in the Asian region, especially the east coast of China and Japan.

Besides the satellite observation, there also have been many studies about the simulation of contrail formation and persistence through the parameterization in a general circulation model (GCM). Early, Schmidt [14] and Appleman [15] provided the thermodynamic explanation of the contrail formation process. According to the Schmidt-Appleman criterion (SAC), further studies [16, 17] pointed out that contrails are usually short-lived once they form in dry ambient air, and if the ambient relative humidity with respect to ice exceeds ice saturation, they can persist at few hours and spread with the ambient wind field and may develop into cirrus clouds. Afterward, Sausen et al. [18] diagnosed the global seasonal contrails coverage from assimilated meteorological data according to a method in a GCM. This method can calculate high cloud coverage from ambient temperature and relative humidity and also can apply SAC to judge the contrail existence when there are aviation activities. A. Schmitt and B. Brunner had provided the data for this method; they use the European Centre for Medium-Range Weather Forecasts (ECMWF) as the meteorological data and the DLR-2 (Deutschen Zentrums für Luft- und Raumfahrt, DLR) data set [19] as the aviation data. The following study Ponater et al. [20] presented the simulated contrail properties and the radiative forcing distribution resulting from contrails. Marquart et al. [21] continually investigated the future development of contrails within a consistent framework, including contrail coverage, contrail properties, and radiative forcing but still limited to line-shaped contrails. Nowadays, the simulation of contrails in a GCM has developed into containing line-shaped contrails and contrail cirrus, while the simulation of contrail coverage or contrail cirrus coverage depends on the calculation of potential contrail coverage (PCC, [22]). The PCC is a method applied to determine the ability of the ambient air to allow contrail formation and consists of SAC and the parameterization of natural cirrus coverage from temperature and humidity in a GCM. Burkhardt and Kärcher [9, 23] and Burkhardt et al., 2015, developed a process-based contrail cirrus module in ECHAM4 to determine contrail formation, persistence, and translation and has used their module to simulate contrail cirrus coverage, the radiative forcing, and related changes in the natural cirrus clouds. Similarly, Rap et al. [24] developed a contrail parameterization by adapting the contrail parameterization of Ponater et al. [20] to the second version of the UK Hadley Centre Global Environmental Model (HadGEM2).

Therefore, we propose one novel object-based contrail detecting method. Based on high temporal resolution imagery of Himawari-8 stationary satellite, it not only detects the contrail occurrence but also reflects the process of contrails persistence and spreading. Different from previous works, we define one new climatological index termed contrail occurrence and persistence (COP). In our statistics experiments, we calculate the fraction of COP with algorithm identification (AI) and artificial visual inspection (AVI), respectively, while analyzing the linear correlation between COP fraction, relative humidity over ice (RHI), and PCC. This paper is organized as follows: Section 2 presents the Himawari-8 satellite and reanalysis data we used. Section 3 illustrates the proposed contrail detection method, the way to calculate the COP index, and PCC parameterization. Section 4 introduces our experimental result and discussion. A brief conclusion is given in Section 5.

2. Data

2.1. Himawari-8 Satellite

Himawari-8 stationary satellite was launched in Oct. 2014. The Advanced Himawari Imager (AHI) on board Himawari-8 is a 16-channel multispectral imagery to capture visible light and infrared images of the Asia-Pacific region. The instrument was designed and built by Exelis Geospatial Systems and has similar spectral and spatial characteristics to the Advanced Baseline Imager (ABI) planned for use in the American GOES-R satellites. The AHI produces images with a resolution down to 500 m and provides full disk observations every 10 mins and the whole Japan territory every 2.5 minutes. Table 1 introduces the characteristics of the Himawari-8 AHI instrument with different channels.


BandCenter wavelengthBandwidthResolution at SSP
(subsatellite point)
Prime measurement objectives and use of sample data

470 nm50 nm1.0 kmDaytime aerosol over land, coastal water mapping
510 nm20 nm1.0 kmGreen band to produce color composite imagery
644 nm30 nm0.5 kmDaytime vegetation/burn scar and aerosols over water, winds
860 nm20 nm1.0 kmDaytime cirrus cloud
1610 nm20 nm2.0 kmDaytime cloud-top phase and particle size, snow
2260 nm20 nm2.0 kmDaytime cloud properties, particle size, vegetation, snow
3.90 µm0.22 µm2.0 kmSurface and cloud, fog at night, fire, winds
6.185 µm0.37 µm2.0 kmHigh-level atmospheric water vapor, winds, rainfall
6.95 µm0.12 µm2.0 kmMid-level atmospheric water vapor, winds, rainfall
7.40 µm0.17 µm2.0 kmLower-level water vapor, winds and SO2
8.50 µm0.32 µm2.0 kmTotal water for stability, cloud phase, dust, SO2, rainfall
9.61 µm0.18 µm2.0 kmTotal ozone, turbulence, winds
10.35 µm0.30 µm2.0 kmSurface and cloud
11.20 µm0.20 µm2.0 kmImagery, SST, clouds, rainfall
12.30 µm0.30 µm2.0 kmTotal water, ash, SST
13.30 µm0.20 µm2.0 kmAir temperature, cloud heights and amounts

2.2. Reanalysis Data

In this paper, we make use of the ECMWF reanalysis data (ERA-Interim, spring in 2016, D. P. Dee et al., 2011). Monthly values of temperature, specific humidity, and ice water content are employed. Horizontally, we have chosen the resolution of variables to a latitude-longitude grid, and vertically we choose 200, 225, 250, and 300 hPa levels, those included the most altitudes of aircraft levels.

3. Method

As shown in Figure 2, our research region is sorted into degree grid boxes extending from 115°E to 144°E and 30°N to 44°N. Three scenes of the Himawari-8 images with different time scales are illustrated in Figure 3, which represent different scenarios to evaluate the proposed contrail detection method. Table 2 presents the information of these Himawari-8 scenes: date and time, spatial extent, and a brief description of contrails.


IDDate and timeSpatial extentScenario description

(a)2017/4/9, 03:20/03:30/03:40118°E–120°E, 34°N–36°NContrails cross with each other
(b)2017/4/4, 03:30/03:40/03:50128°E–130°E, 42°N–44°NContrails lie closely with each other
(c)2017/3/31, 00:10/00:40/01:00126°E–132°E, 32°N–38°NContrails are densely distributed in the image

3.1. Contrail Detection Method

Different from traditional CDA method and its variants only considering the spectral information of the image, our work focuses on the object-based method for the detecting contrails in each grid box of Himawari-8 images as shown in Figure 2. The main process consists of the following two steps.

3.1.1. Multiresolution Segmentation

In our method, objects in Himawari-8 images are divided into different groups based on contrast, similarity, and shape of object, which are termed heterogeneity. There are several basic steps in the multiresolution segmentation procedure.(1)The first step of segmentation procedure is to define a single pixel as the starting point.(2)The single pixel fuses with other pixels as one group, if they are within the threshold of heterogeneity criteria.(3)Pixel groups fuse with those neighbor groups.(4)All of the pixels have been assigned to different objects until no further fusing is found.

3.1.2. Object-Based Classification

A nearest neighbor classification method is adopted to identify the Himawari-8 image into two classes: contrail and noncontrail object after multiresolution segmentation:(1)It assigns several samples with contrail and noncontrail label, respectively. Objects should be verified with shape, size, and spectral characteristics.(2)Contrail and noncontrail samples are trained from the segmented objects. Contrail and noncontrail classes are linked with the segmented image objects using the k-nearest neighbor classification method.(3)Classification returns a fuzzy membership value for all the segmented image objects. A value of 0 means the object does not belong to contrail class, while a value of 1 means the object most likely belongs to contrail class.

3.2. Artificial Visual Analysis

With the high temporal resolution stationary satellite images, we not only explore the occurrence of linear contrail but also study the development from linear contrail to contrail cirrus. In our evaluation, we investigate the satellite images of spring 2016 (March, May, and April) in our statistics analysis. After a large amount of observation analysis, we choose 30 min as the time scale of statistic, so as to avoid the overestimation of contrail, as well as fully considering the spreading of contrails. Thus, 4416 satellite images (24 per day and 92 days) are analyzed with both the proposed contrail detection method and artificial visual inspection. In the previous studies [1, 2527], the reconstruction of contrail occurrence fraction adopts commercial flight track data to mask out regions of no air traffic. Their work has obvious limitations as follows:(1)The polar satellite overpasses the observed region twice per day, which cause the severe insufficiency in observation sample.(2)This kind of reconstruction did not consider the contrail spreading and persistence, with limited observation sample.

Based on a very large amount of observation, some contrails could persist more than 5 h and spread 400–500 km at most, according to the annual mean wind speed at 200–300 hPa. Thus we define one new climatological index, termed contrail occurrence and persistence (COP). First, each of the grid boxes in satellite images is divided into 8 × 8 subgrid boxes; the COP is the ratio between the number of subgrids that contain detected contrails and the total number of subgrids, as illustrated in Figure 4. Different from the traditional climatological index of contrail based on limited satellite overpass images, the COP index will count and aggregate detected contrails with 30 min time interval, which will reflect the occurrence and persistence of contrail.

3.3. Relative Humidity over Ice (RHI)

The contrails occurrence fraction presents a significant linear correlation versus the RHI on North America [25]. Therefore, for the comparison between the contrails occurrence fraction versus RHI on East Asia, we use the reanalysis data of temperature to calculate RHI by a formula as follows:where is the specific humidity, is the saturation specific humidity over ice, and is the saturation pressure of water vapor over ice and calculated by an empirical formula as follows:

3.4. Potential Contrail Coverage (PCC) Parameterization

Contrail formation depends on the surrounding temperature, moisture, and pressure fields that create an enough cold and moist ambient air for the mixing between the aircraft exhaust plume and its environment. Besides, we use SAC to diagnose the condition of ambient air with persistent contrails [16, 17]. The PCC is a method applied to determine the ability of the ambient air to allow contrail formation. An introduction necessary for PCC to estimate contrail coverage requires the fractional area of the atmosphere to support a persistent contrail formation [20]. Hence, in this paper, we adopt a similar method of PCC parameterization developed by Ponater et al. [20] for the ECHAM4 climate model. Relying on the thermodynamic theory, an empirical formula of the threshold values of temperature () and relative humidity () supporting contrail formation and persistence has been given according to Schumann [16]. In addition, contrail formation and persistence depend on some specific parameters and variables including the ambient temperature (), pressure (), specific humidity (), the emission index of water vapor (), the specific heat of fuel combustion (), and the propulsion efficiency of the aircraft (). The thermodynamic theory predicts threshold values for temperature () and humidity (). No contrails are possible if and . The formula of (in °C) is given by the following:where is the slope of the mean phase trajectory in the turbulent exhaust field on an absolute temperature versus water vapor partial pressure diagram and has the unit of Pa K−1, defined as follows:where , is the ratio of molecular masses of water and dry air,  J kg−1 K−1, , and is the isobaric heat capacity of moist air, which has the unit of J kg−1 K−1 and is given by the following:where  J kg−1 K−1 is the isobaric heat capacity of dry air and  J kg−1 K−1 is the isobaric heat capacity of water vapor. Hence, is a function of , not a constant. The critical relative humidity can be calculated by , , and the ambient temperature as follows:where is the saturation pressure of water vapor over water and is given by:Following the Ponater et al. [20] study, we define a modified threshold for contrail formation by combining with the threshold . Here is a critical threshold value that indicates a minimum relative humidity necessary to allow cloud formation within a grid box:

because the PCC consists of SAC and the parameterization of natural cirrus coverage from temperature and humidity. In this paper, we adopt two different kinds of the parameterization of natural cirrus coverage to calculate and obtain two kinds of PCC fraction. One of the natural cirrus cloud coverage () from contrail parameterization in HadGEM2 is given by (Smith, 1990) the following:where is defined bywhere is the ice water content, , is the saturation specific humidity and is the relative humidity over water. We employ from (8) into (10) instead of and adopt the same : Meanwhile we also define and plunge into (9) instead of . Therefore we obtain a potential cloud coverage for all high clouds (), which includes both nature cirrus and contrails. The first potential coverage for contrails called PCC1 could be calculated by

Another the natural cirrus cloud coverage () from contrail parameterization in ECHAM4 is also given by (Sudqvist et al., 1989) the following:where is the relative humidity over ice in (13). Similarly, we can obtain by replacing with in (13). We use this parameterization of natural cirrus coverage to define a potential coverage for contrails called PCC2 asHowever, calculated in this way is a three-dimensional field (longitude × latitude × level), so considering how to integrate a two-dimensional PCC field (longitude × latitude) over all 4 levels (from 200 hPa to 300 hPa), we adopt the maximum/random overlap assumption as described by Geleyn and Hollingsworth (1978).

4. Result and Discussion

4.1. Contrails Detection

Figure 5 shows the results of the detection using the proposed method in the different scenarios. The images were classified into two classes of contrail and noncontrail. The red area was classified as contrail and the blue area was classified as noncontrail. However, the contrails have still been broken into several parts and are disconnected with each other. As labeled in green cycle, there are some false alarms about contrail. Some misdetection happened and was labeled with the black cycle. The goal of contrail detection methods is to obtain a low false alarm rate (FAR) with sufficient detection efficiency (DE). Sensitivity of the algorithm depends on the thermal homogeneity and land/ocean contrast with contrail. Detection efficiency suffers from underestimation of contrail width and contrail cirrus overlap, while the algorithm cannot detect weak contrail structures that can still be seen by the human eye. Because of several uncertainties of algorithm identification, we also employ the artificial visual inspection to compute the COP fraction.

4.2. Plots of the COP Fraction versus the RHI and PCC

Figure 6(a) presents the statistical COP fractions according to AI, while Figure 6(b) shows the statistical COP fractions derived from AVI. Although the general distribution of COP is similar to AVI, the AI field has obviously lower COP values than the AVI field because AI is hard to detect apotypic contrails like wide spread and fusion with natural cirrus. Due to the low spatial resolution, natural cirrus clouds with a linear appearance are also usually misclassified as contrails. The high rate of misdetections can be avoided by using higher spatial resolution satellite data. In our experiments, both the AI and AVI fields have broad maxima over east China’s Shandong, Anhui, and Jiangsu Province, minima over the sea of Japan and north of Korean Peninsula, another area of broad maxima around the Korean Strait and over the Yellow Sea, east of Japan’s Honshu Island. In addition, Figure 6(c) shows that the obvious difference between AI and AVI fields has broad large values over the region where AI and AVI fields have the similar large values. The reason for the difference should be that the linear or slightly bent shape of contrails is more easily identifiable by AVI. Although AI can identify more linear contrails over concentrated areas, the density of linear contrails identified by AVI is higher than AI over concentrated areas. It is reasonable that these obvious differences appear in the concentrated areas of linear contrails. However, we can reduce huge amount of statistical work through AI, and AVI has higher accuracy but shows powerless facing to massive satellite imagery processing, which is the reason that we only choose one season and a part of East Asia as the research time and area, respectively.

As shown in Figure 7, plots of the COP fractions versus the mean of RHI, PCC1, and PCC2 values calculated in grid box. Figures 7(a), 7(c), and 7(e) show the relationship between COP and variables for AI, and Figures 7(b), 7(d), and 7(f) show the same content for AVI. The Pearson correlation coefficients between COP and variables are presented in Table 3. As illustrated in Table 3 and Figure 7, there is a strong correlation between COP and RHI, corresponding to 0.72 for AVI, which is better than AI. And, it is obvious that the correlation coefficients for RHI are correspondingly greater than those for PCCs. In addition, PCC1’s linear correlations are clearly better than those for PCC2.


RHIPCC1PCC2

AI COP
AVI COP

Note. The double asterisks represent statistically significant values at 99% confidence level.

Contrails cause an alteration in the earth’s radiation budget, via their shortwave (SW) albedo effect and longwave (LW) greenhouse effect to impact climate. Contrail coverage and optical depth are essential aspects about contrail radiative forcing. Thus PCC1 (Smith 1990) reflect the actual reflection of contrail coverage better than PCC2 (Sudqvist et al., 1989) in model simulation, based on our observations and comparison.

5. Conclusion

Contrails are important for understanding how the humans contribute to climate change by one artificial element into the atmosphere. Identifying contrails is the first step in contrail relative study. In this paper, object-based contrail detecting method is proposed to reflect the process of contrail occurrence and persistence. According to the algorithm identification (AI) and artificial visual inspection (AVI), COP measured from Himawari-8 stationary satellite imagery is related to upper tropospheric relative humidity over ice (RHI) computed with the ECMWF reanalysis data by simple linear regression. Two kinds of potential contrail coverage (PCC1 and PCC2), from contrail parameterization in ECHAM4 and HadGEM2, are compared with distribution of COP. Through the linear correlation between COP and PCCs fractions, we found the PCC1 has better correspondence with COP, which means that the PCC1 in model simulation reflects the distribution of actual contrails better than PCC2.

Disclosure

This paper is also a contribution (no. 179) to the ESMC of NUIST.

Conflicts of Interest

The authors declare that they have no conflicts of interest.

Acknowledgments

This work was carried out with the Scientific Research Foundation (Grant no. S8113055001) of Nanjing University of Information Science and Technology, Natural Science Foundation of Jiangsu Province (Grant no. BK20150931), Natural Science Foundation of China (Grants no. 61702275 and no. 41775008), and Priority Academic Program Development of Jiangsu Higher Education Institutions (PAPD).

References

  1. D. P. Duda, P. Minnis, K. Khlopenkov, T. L. Chee, and R. Boeke, “Estimation of 2006 Northern Hemisphere contrail coverage using MODIS data,” Geophysical Research Letters, vol. 40, no. 3, pp. 612–617, 2013. View at: Publisher Site | Google Scholar
  2. C. Liu, P. Yang, P. Minnis et al., “A two-habit model for the microphysical and optical properties of ice clouds,” Atmospheric Chemistry and Physics, vol. 14, no. 24, pp. 13719–13737, 2014. View at: Publisher Site | Google Scholar
  3. F. Zhang, K. Wu, J. Li, Q. Yang, J.-Q. Zhao, and J. Li, “Analytical infrared delta-four-stream adding method from invariance principle,” Journal of the Atmospheric Sciences, vol. 73, no. 10, pp. 4171–4188, 2016. View at: Publisher Site | Google Scholar
  4. F. Zhang and J. Li, “A note on double Henyey–Greenstein phase function,” Journal of Quantitative Spectroscopy and Radiative Transfer, vol. 184, pp. 40–43, 2016. View at: Publisher Site | Google Scholar
  5. E. J. Jensen, O. B. Toon, S. A. Vay et al., “Prevalence of ice-supersaturated regions in the upper troposphere: implications for optically thin ice cloud formation,” Journal of Geophysical Research Atmospheres, vol. 106, no. 15, Article ID 2000JD900526, pp. 17253–17266, 2001. View at: Publisher Site | Google Scholar
  6. F. Zhang, Y.-N. Shi, J. Li, K. Wu, and H. Iwabuchi, “Variational iteration method for infrared radiative transfer in a scattering medium,” Journal of the Atmospheric Sciences, vol. 74, no. 2, pp. 419–430, 2017. View at: Publisher Site | Google Scholar
  7. F. Zhang, Y. Lei, J.-R. Yan, J.-Q. Zhao, J. Li, and Q. Dai, “A new parameterization of canopy radiative transfer for land surface radiation models,” Advances in Atmospheric Sciences, vol. 34, no. 5, pp. 613–622, 2017. View at: Publisher Site | Google Scholar
  8. F. Zhang, K. Wu, P. Liu, X. Jing, and J. Li, “Accounting for Gaussian quadrature in four-stream radiative transfer algorithms,” Journal of Quantitative Spectroscopy and Radiative Transfer, vol. 192, pp. 1–13, 2017. View at: Publisher Site | Google Scholar
  9. U. Burkhardt and B. Kärcher, “Global radiative forcing from contrail cirrus,” Nature Climate Change, vol. 1, no. 1, pp. 54–58, 2011. View at: Publisher Site | Google Scholar
  10. H. Hetzheim, “Automated contrail and cirrus detection using stochastic properties,” International Journal of Remote Sensing, vol. 28, no. 9, pp. 2033–2048, 2007. View at: Publisher Site | Google Scholar
  11. P. Minnis, R. Palikonda, B. J. Walter, J. K. Ayers, and H. Mannstein, “Contrail properties over the eastern North Pacific from AVHRR data,” Meteorologische Zeitschrift, vol. 14, no. 4, pp. 515–523, 2005. View at: Publisher Site | Google Scholar
  12. R. Meyer, H. Mannstein, R. Meerkötter, U. Schumann, and P. Wendling, “Regional radiative forcing by line-shaped contrails derived from satellite data,” Journal of Geophysical Research: Atmospheres, vol. 107, no. 10, article 4104, 2002. View at: Publisher Site | Google Scholar
  13. D. P. Duda, P. Minnis, L. Nguyen, and R. Palikonda, “A case study of the development of contrail clusters over the Great Lakes,” Journal of the Atmospheric Sciences, vol. 61, no. 10, pp. 1132–1146, 2004. View at: Publisher Site | Google Scholar
  14. E. Schmidt, “Die entstehung von eisnebel aus den auspuffgasen von flugmotoren,” in Schriften der Deutschen Akademie der Luftfahrtforschung, Kommissionsverlag von R. Oldenbourg, Munchen, Germany, 1941, Heft 44, 5:1-15. View at: Google Scholar
  15. H. Appleman, “The formation of exhaust condensation trails by jet aircraft,” Bulletin of the American Meteorological Society, vol. 34, pp. 14–20, 1953. View at: Google Scholar
  16. U. Schumann, “On conditions for contrail formation from aircraft exhausts,” Meteorologische Zeitschrift, vol. 5, no. 1, pp. 4–23, 1996. View at: Google Scholar
  17. U. Schumann, “Influence of propulsion efficiency on contrail formation,” Aerospace Science and Technology, vol. 4, no. 6, pp. 391–401, 2000. View at: Publisher Site | Google Scholar
  18. R. Sausen, K. Gierens, M. Ponater, and U. Schumann, “A diagnostic study of the global distribution of contrails Part I: present day climate,” Theoretical and Applied Climatology, vol. 61, no. 3-4, pp. 127–141, 1998. View at: Publisher Site | Google Scholar
  19. A. Schmitt and B. Brunner, “Emissions from aviation and their development over time, llutants from Air Traffic-Results of Atmospheric Research 1992-1997,” DLR Mitteilung, vol. 97, no. 04, pp. 37–52, 1997. View at: Google Scholar
  20. M. Ponater, S. Marquart, and R. Sausen, “Contrails in a comprehensive global climate model: parameterization and radiative forcing results,” Journal of Geophysical Research Atmospheres, vol. 107, no. 13, pp. 1–15, 2002. View at: Publisher Site | Google Scholar
  21. S. Marquart, M. Ponater, F. Mager, and R. Sausen, “Future development of contrail cover, optical depth, and radiative forcing: impacts of increasing air traffic and climate change,” Journal of Climate, vol. 16, no. 17, pp. 2890–2904, 2003. View at: Publisher Site | Google Scholar
  22. U. Burkhardt, B. Kärcher, M. Ponater, K. Gierens, and A. Gettelman, “Contrail cirrus supporting areas in model and observations,” Geophysical Research Letters, vol. 35, no. 16, Article ID L16808, 2008. View at: Publisher Site | Google Scholar
  23. U. Burkhardt and B. Kärcher, “Process-based simulation of contrail cirrus in a global climate model,” Journal of Geophysical Research Atmospheres, vol. 114, no. 16, Article ID D16201, 2009. View at: Publisher Site | Google Scholar
  24. A. Rap, P. M. Forster, A. Jones et al., “Parameterization of contrails in the UK Met Office climate model,” Journal of Geophysical Research Atmospheres, vol. 115, no. 10, Article ID D10205, 2010. View at: Publisher Site | Google Scholar
  25. D. P. Duda, P. Minnis, and L. A. Avey, “Towards improved contrail parameterizations for climate-scale models,” in Proceedings of the 13th Conference on Aviation, Range and Aerospace Meteorology, New Orleans, La, USA, 2008. View at: Google Scholar
  26. S. Gao, B. Chen, T. Li, N. Wu, and W. Deng, “AIRS-observed warm core structures of tropical cyclones over the western North Pacific,” Dynamics of Atmospheres and Oceans, vol. 77, pp. 100–106, 2017. View at: Publisher Site | Google Scholar
  27. S. Gao, S. Zhai, L. S. Chiu, and D. Xia, “Satellite air-sea enthalpy flux and intensity change of tropical cyclones over the western North Pacific,” Journal of Applied Meteorology and Climatology, vol. 55, no. 2, pp. 425–444, 2016. View at: Publisher Site | Google Scholar

Copyright © 2017 Jinglin Zhang et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.


More related articles

 PDF Download Citation Citation
 Download other formatsMore
 Order printed copiesOrder
Views1040
Downloads351
Citations

Related articles

We are committed to sharing findings related to COVID-19 as quickly as possible. We will be providing unlimited waivers of publication charges for accepted research articles as well as case reports and case series related to COVID-19. Review articles are excluded from this waiver policy. Sign up here as a reviewer to help fast-track new submissions.