EFFECT OF ATMOSPHERIC OVERLAPPING BANDS AND THEIR TREATMENT ON THE CALCULATION OF THERMAL RADIATION

Shi Guangyu

doi:10.1007/BF02678137

Impact Factor: 5.8

Volume 1 Issue 2

Jul. 1984

Article Contents

Article > ADVANCES IN ATMOSPHERIC SCIENCES > 1984 > 1(2): 246-262

EFFECT OF ATMOSPHERIC OVERLAPPING BANDS AND THEIR TREATMENT ON THE CALCULATION OF THERMAL RADIATION

Shi Guangyu

1.
InstituteofAtmosphericPhysics,AcademiaSinica,Beijing

Shi Guangyu

doi: 10.1007/BF02678137

Abstract
References
Related papers
PDF

Abstract:
The effect of the overlapping band of atmospheric gases and its treatment on the calculation of flux and cooling rate due to the long wave radiation is investigated in detail by a new transmission model for overlapping bands, taking the 15 μm band of CO2 as an example. It is found that the presence of band overlapping has a quite significant influence on radiative fluxes and cooling rates in the upper stratosphere and the troposphere, in particular, at the earth's surface. However, in the middle-lower stratosphere, the overlapping effect appears to be insignificant. It is also shown that the usual wide-band transmission model treating the overlapping effect overestimates the net longwave fluxes in the lower stratosphere and, in particular, in the troposphere including the surface. But, in the middle-upper stratosphere, the contrary is the case.
References

[1]	Shi Guangyu, Qu Yanni, 1986: EFFECTS OF RADIATION MODELS ON THE CALCULATION OF ATMOSPHERIC INFRARED COOLING RATES, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 227-237. doi: 10.1007/BF02682556
[2]	HUANG Hong, JIANG Yongqiang, CHEN Zhongyi, LUO Jian, WANG Xuezhong, 2014: Effect of Tropical Cyclone Intensity and Instability on the Evolution of Spiral Bands, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 1090-1100. doi: 10.1007/s00376-014-3108-5
[3]	Bao Ning, Zhang Xuehong, 1991: Effect of Ocean Thermal Diffusivity on Global Warming Induced by Increasing Atmospheric CO2, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 421-430. doi: 10.1007/BF02919265
[4]	HUANG Sixun, CAO Xiaoqun, DU Huadong, WANG Tingfang, XIANG Jie, 2006: Retrieval of Atmospheric and Oceanic Parameters and the Relevant Numerical Calculation, ADVANCES IN ATMOSPHERIC SCIENCES, 23, 106-117. doi: 10.1007/s00376-006-0011-8
[5]	Zhang Fengying, Ma Xialin, 1986: CALCULATION OF UPDATED COEFFICIENTS FOR ATMOSPHERIC TEMPERATURE RETRIEVAL, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 150-161. doi: 10.1007/BF02682549
[6]	Zhao Ping, Chen Longxun, 2000: Calculation of Solar Albedo and Radiation Equilibrium over the Qinghai-Xizang Plateau and Analysis of Their Climatic Features, ADVANCES IN ATMOSPHERIC SCIENCES, 17, 140-156. doi: 10.1007/s00376-000-0050-5
[7]	Qian Yongfu, 1987: RECURRENCE METHOD FOR CALCULATION OF ATMOS-PHERIC COOLING RATE DUE TO INFRARED RADIATION, ADVANCES IN ATMOSPHERIC SCIENCES, 4, 403-413. doi: 10.1007/BF02656741
[8]	Qiu Jinhuan, Wang Kaixiang, 1993: A Study of the Radiation-Climate Effect of Aerosol over Beijing Area, ADVANCES IN ATMOSPHERIC SCIENCES, 10, 147-154. doi: 10.1007/BF02919137
[9]	Zhao Bolin, Zhang Xiaoli, Zhu Yuanjing, 1992: Study on Cloud-Radiation Effect on Climate in Eastern Asia, ADVANCES IN ATMOSPHERIC SCIENCES, 9, 257-268. doi: 10.1007/BF02656936
[10]	WANG Lu, and YANG Haijun, 2014: The Role of Atmospheric Teleconnection in the Subtropical Thermal Forcing on the Equatorial Pacific, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 985-994. doi: 10.1007/s00376-013-3173-1
[11]	Chen Yuejuan, H. L. Kuo, 1986: A GLOBAL MODEL WITH OVERLAPPING MERCATOR AND STEREOGRAPHIC GRIDS, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 302-313. doi: 10.1007/BF02678651
[12]	Zhenhui WANG, Xinxiu SUI, Qing ZHANG, Lu YANG, Hang ZHAO, Min TANG, Yizhe ZHAN, Zhiguo ZHANG, 2017: Derivation of Cloud-Free-Region Atmospheric Motion Vectors from FY-2E Thermal Infrared Imagery, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 272-282. doi: 10.1007/s00376-016-6098-7
[13]	SHANG Lin, LIU Yi, TIAN Wenshou, ZHANG Yuli, 2015: Effect of Methane Emission Increases in East Asia on Atmospheric Circulation and Ozone, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 1617-1627. doi: 10.1007/s00376-015-5028-4
[14]	Chen Wuhe, Situ Da, Zhong Xubin, 1998: Atmospheric Refractive Turbulence Effect on Diffraction-Limited Infrared Coherent Lidar, ADVANCES IN ATMOSPHERIC SCIENCES, 15, 124-134. doi: 10.1007/s00376-998-0024-6
[15]	Jia Xinyuan, 1997: The Effect of Mesoscale Flows on Regional Atmospheric Transport in a Complex Terrain, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 535-540. doi: 10.1007/s00376-997-0071-4
[16]	Liu Chunlei, Yao Keya, 1996: Calculation of Ice Crystal Diffraction, ADVANCES IN ATMOSPHERIC SCIENCES, 13, 340-348. doi: 10.1007/BF02656851
[17]	Cheng Minghu, Shi Guangyu, Zhou Xiuji, 1990: Numerical Experiment of Combined Infrared and Ultraviolet Radiation Remote Sensing to Determine the Profile and Total Content of Atmospheric Ozone, ADVANCES IN ATMOSPHERIC SCIENCES, 7, 305-319. doi: 10.1007/BF03179763
[18]	Wenshou TIAN, GUO Zhenhai, YU Rucong, 2004: Treatment of LBCs in 2D Simulation of Convection over Hills, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 573-586. doi: 10.1007/BF02915725
[19]	Jinqiang ZHANG, Hongbin CHEN, Xiang'ao XIA, Wei-Chyung WANG, 2016: Dynamic and Thermodynamic Features of Low and Middle Clouds Derived from Atmospheric Radiation Measurement Program Mobile Facility Radiosonde Data at Shouxian, China, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 21-33. doi: 10.1007/s00376-015-5032-8
[20]	WANG Aihui, ZENG Xubin, 2009: Improving the Treatment of the Vertical Snow Burial Fraction over Short Vegetation in the NCAR CLM3, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 877-886. doi: 10.1007/s00376-009-8098-3

PDF

Get Citation+

Export:

Article Metrics

Article Views: 1273 Times

PDF downloads: 1065 Times

Cited by: Times

Proportional views

Manuscript History

Manuscript received: 10 July 1984

Manuscript revised: 10 July 1984

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

EFFECT OF ATMOSPHERIC OVERLAPPING BANDS AND THEIR TREATMENT ON THE CALCULATION OF THERMAL RADIATION

Shi Guangyu

1. InstituteofAtmosphericPhysics,AcademiaSinica,Beijing

Manuscript received: 1984-07-10
Manuscript revised: 1984-07-10

Abstract: The effect of the overlapping band of atmospheric gases and its treatment on the calculation of flux and cooling rate due to the long wave radiation is investigated in detail by a new transmission model for overlapping bands, taking the 15 μm band of CO2 as an example. It is found that the presence of band overlapping has a quite significant influence on radiative fluxes and cooling rates in the upper stratosphere and the troposphere, in particular, at the earth's surface. However, in the middle-lower stratosphere, the overlapping effect appears to be insignificant. It is also shown that the usual wide-band transmission model treating the overlapping effect overestimates the net longwave fluxes in the lower stratosphere and, in particular, in the troposphere including the surface. But, in the middle-upper stratosphere, the contrary is the case.