基于瑞利激光雷达对格尔木地区中间层逆温层特征分析

乔帅; 潘蔚琳; 班超; 陈磊; 鱼艇

doi:10.11728/cjss2019.01.084

基于瑞利激光雷达对格尔木地区中间层逆温层特征分析

doi: 10.11728/cjss2019.01.084

乔帅^1,2,
潘蔚琳^1,2,
班超¹,
陈磊^1,2,
鱼艇³

1. 中国科学院大气物理研究所北京 100029;
2. 中国科学院大学北京 100049;
3. 中国洛阳电子装备试验中心济源 459000

基金项目:

国家自然科学基金项目资助（41127901）

详细信息

作者简介:
乔帅,panweilin@mail.iap.ac.cn

中图分类号: P356
计量
- 文章访问数: 935
- HTML全文浏览量: 106
- PDF下载量: 342
- 被引次数: 0
出版历程
- 收稿日期: 2018-01-16
- 修回日期: 2018-08-06
- 刊出日期: 2019-01-15

Characterization of Mesospheric Inversion Layer with Rayleigh Lidar Data over Golmud

1 Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029;
2 University of Chinese Academy of Sciences, Beijing 100049;
3 Luoyang Electronic Equipment Test Center of China, Jiyuan 459000

摘要

摘要: 利用MARMOT （Middle Atmosphere Remote Mobile Observatory in Tibet）激光雷达对2014年7月至12月格尔木（36.25°N，94.54°E）上空的中间层逆温层MIL （Mesosphere Inversion Layer）事件进行研究分析.格尔木MIL现象的发生频率为53.8%，其中冬季（12月）发生频率最高，达76%；秋季（9-10月）较高，为60%；夏季（7-8月）发生频率较低，为29%.2014年7月至12月观测到的MIL逆温幅度主要分布在5～20K，平均逆温幅度为15.9K.秋季逆温层底部高度较高，主要分布在77～84km，冬季和夏季逆温层底部高度较低，主要分布在64～74km.逆温层底部高度平均为75.1km.逆温层的平均宽度为8.7km，由夏季到冬季呈递增趋势.
- 激光雷达 /
- 中间层 /
- 逆温层
Abstract: Based on the measurements of MARMOT (Middle Atmosphere Remote Mobile Observatory in Tibet) lidar located in Golmud, Qinghai (36.25°N, 94.54°E) from July to December 2014, Mesospheric Inversion Layer (MIL) over Golmud area has been analyzed. The average occurrence frequency of MIL over Golmud is 53.8% during this period. The occurrence frequency is highest and can be up to 76% in winter (December), is around 60% in autumn equinox, and is as low as 29% in summer (July, August). The amplitude of temperature inversion is within 5~20K, and the average value is 15.9K. The mean bottom altitude of MIL is 75.1km. The bottom altitude is higher and mainly from 77 to 84km in autumn. It is lower in winter and summer, and mainly from 64 to 74km. The mean width of MIL is 8.7km, and it increases from summer to winter.
- Lidar /
- Mesosphere /
- Mesospheric Inversion Layer (MIL)

HTML全文

参考文献(36)

[1]	MERIWETHER J W, GERRARD A J. Mesosphere inversion layers and stratosphere temperature enhancements[J]. Rev. Geophys., 2004, 42(3):1-31
[2]	SCHMIDLIN F J. Temperature inversions near 75km[J]. Geophys. Res. Lett., 1976, 3(3):173-176
[3]	LÜBKEN F J, HILLERT W, LEHMACHER G, et al. Intercomparison of density and temperature profiles obtained by lidar, ionization gauges, falling spheres, datasondes and radiosondes during the DYANA campaign[J]. J. Atmos. Terr. Phys., 1994, 56(13-14):1969-1984
[4]	LEBLANC T, HAUCHECORNE A. Recent observations of mesospheric temperature inversions[J]. J. Geophys. Res.:Atmos., 1997, 102(D16):19471-19482
[5]	FADNAVIS S, BEIG G. Mesospheric temperature inversions over the Indian tropical region[J]. Ann. Geophys., 2004, 22(10):3375-3382
[6]	CHEN Linxiang, YANG Guotao, WANG Jihong, et al. Measurements of lower mesosphere inversion layers with rayleigh lidar over Beijing[J]. Chin. J. Space Sci., 2017, 37(1):75-81(陈林祥, 杨国韬, 王继红, 等. 瑞利激光雷达探测北京上空中间层低逆温层[J]. 空间科学学报, 2017, 37(1):75-81)
[7]	SHE C Y, YU J R, CHEN H. Observed thermal structure of a midlatitude mesopause[J]. Geophys. Res. Lett., 1993, 20(7):567-570
[8]	STATES R J, GARDNER C S. Influence of the diurnal tide and thermospheric heat sources on the formation of mesospheric temperature inversion layers[J]. Geophys. Res. Lett., 1998, 25(9):1483-1486
[9]	HUANG T Y, HICKEY M P, TUAN T F, et al. Further investigations of a mesospheric inversion layer observed in the ALOHA-93 Campaign[J]. J. Geophys. Res. Atmos., 2002, 107(D19):ACL 17-1-ACL 17-8
[10]	YUAN T, PAUTET P D, ZHAO Y, et al. Coordinated investigation of midlatitude upper mesospheric temperature inversion layers and the associated gravity wave forcing by Na lidar and advanced mesospheric temperature mapper in Logan, Utah[J]. J. Geophys. Res.:Atmos., 2014, 119(7):3756-3769
[11]	CLANCY R T, RUSCH D W, CALLAN M T, et al. Temperature minima in the average thermal structure of the middle mesosphere (70~80km) from analysis of 40-to 92-km SME global temperature profiles[J]. J. Geophys. Res.:Atmos., 1994, 99(D9):19001-19020
[12]	GAN Q, ZHANG S D, YI F. TIMED/SABER observations of lower mesospheric inversion layers at low and middle latitudes[J]. J. Geophys. Res.:Atmos., 2012, 117(D7):1-14
[13]	MERIWETHER J W, GARDNER C S. A review of the mesosphere inversion layer phenomenon[J]. J. Geophys. Res.:Atmos., 2000, 105(D10):12405-12416
[14]	DUCK T J, SIPLER D P, SALAH J E, et al. Rayleigh lidar observations of a mesospheric inversion layer during night and day[J]. Geophys. Res. Lett., 2001, 28(18):3597-3600
[15]	HAUCHECORNE A, MAILLARD A. A 2-d dynamical model of mesospheric temperature inversions in winter[J]. Geophys. Res. Lett., 1990, 17(12):2197-2200
[16]	SASSI F, GARCIA R R, BOVILLE E, et al. On temperature inversions and the mesospheric surf zone[J].J. Geophys. Res.:Atmos., 2002, 107(D19):ACL 8-1-ACL 8-11
[17]	SICA R J, ARGALL P S, SHEPHERD T G, et al. Model-measurement comparison of mesospheric temperature inversions, and a simple theory for their occurrence[J]. Geophys. Res. Lett., 2007, 34(23):231-247
[18]	FADNAVIS S, SⅡNGH D, BEIG G, et al. Seasonal variation of the mesospheric inversion layer, thunderstorms, and mesospheric ozone over India[J]. J. Geophys. Res.:Atmos., 2007, 112(D15):1-12
[19]	QIAO S, PAN W, ZHU K Y, et al. Initial results of lidar measured middle atmosphere temperatures over tibetan plateau[J]. Atmos. Oceanic Sci. Lett., 2014, 7(3):213-217
[20]	YU Ting, PAN Weilin, ZHU Keyun, et al. Preliminary analysis of mesospheric summer temperature measurements in Golmud[J]. Infrared Laser Eng., 2016, 45(12):1211005-1-1211005-7(鱼艇, 潘蔚琳, 朱克云, 等. 夏季格尔木中间层大气温度探测初步分析[J]. 红外与激光工程, 2016, 45(12):1211005-1-1211005-7)
[21]	MERTENS C J, MLYNCZAK M J, LÓPEZ-PUERTAS M, et al. Retrieval of mesospheric and lower thermospheric kinetic temperature from measurements of CO₂ 15μm earth limb emission under non-LTE conditions[J]. Geophys. Res. Lett., 2001, 28(7):1391-1394
[22]	PICONE J M, HEDIN A E, DROB D P, et al. NRLMSISE-00 empirical model of the atmosphere:Statistical comparisons and scientific issues[J]. J. Geophys. Res.:Space Phys., 2002, 107(A12):SIA 15-1-SIA 15-16
[23]	QIAO S, PAN W L, LÜ D. Winter mesospheric thermal structure over tibetan plateau[C]//The 27th International Laser Radar Conference 2016. New York, USA, 2016
[24]	HAUCHECORNE A, CHANIN M L, WILSON R. Mesospheric temperature inversion and gravity wave breaking[J]. Geophys. Res. Lett., 1987, 14(9):933-936
[25]	WHITEWAY J A, CARSWELL A I, WARD W E. Mesospheric temperature inversions with overlying nearly adiabatic lapse rate:An Indication of a well-mixed turbulent layer[J]. Geophys. Res. Lett., 1995, 22(10):1201-1204
[26]	GILLE S T, HAUCHECORNE A, CHANIN M L. Semidiurnal and diurnal tidal effects in the middle atmosphere as seen by Rayleigh lidar[J]. J. Geophys. Res.:Atmos., 1991, 96(D4):7579-7587
[27]	STATES R J, GARDNER C S. Thermal structure of the mesopause region (80~105km) at 40°N latitude. Part Ⅱ:Diurnal Variations[J]. J. Atmos. Sci., 2000, 57(1):66-77
[28]	RAMESH K, SRIDHARAN S. Large mesospheric inversion layer due to breaking of small-scale gravity waves:evidence from rayleigh lidar observations over Gadanki (13.5°N, 79.2°E)[J]. J. Atmos. Sol.-Terr. Phys., 2012, 89(89):90-97
[29]	RAMESH K, SRIDHARAN S, RAGHUNATH K, et al. Planetary wave-gravity wave interactions during mesospheric inversion layer events[J]. J. Geophys. Res. Space Phys., 2013, 118(7):4503-4515
[30]	GARDNER C S, YANG W M. Measurements of the dynamical cooling rate associated with the vertical transport of heat by dissipating gravity waves in the mesopause region at the Starfire Optical Range, New Mexico[J]. J. Geophys. Res. Atmos., 1998, 103(D14):16909-16926
[31]	LIU H L, HAGAN M E. Local heating/cooling of the mesosphere due to gravity wave and tidal coupling[J]. Geophys. Res. Lett., 1998, 25(15):2941-2944
[32]	LIU H L, HAGAN M E, ROBLE R G. Local mean state changes due to gravity wave breaking modulated by the diurnal tide[J]. J. Geophys. Res.:Atmos., 2000, 105(D10):12381-12396
[33]	BROWN L B, GERRARD A J, MERIWETHER J W, et al. All-sky imaging observations of mesospheric fronts in OI 557.7nm and broadband OH airglow emissions:Analysis of frontal structure, atmospheric background conditions, and potential sourcing mechanisms[J]. J. Geophys. Res.:Atmos., 2004, 109(D19):1-19
[34]	MLYNCZAK M G, MORGAN F, YEE J H, et al. Simultaneous measurements of the O2(^1Δ) and O2(^1Σ) Airglows and ozone in the daytime mesosphere[J]. Geophys. Res. Lett., 2001, 28(6):999-1002
[35]	XU Xiaohua, GUO Jincheng, LUO Jia. Analysis of the active characteristics of stratosphere gravity waves over the Qinghai-Tibetan Plateau using COSMIC radio occultation data[J]. Chin. J. Geophys., 2016, 59(4):1199-1210(徐晓华, 郭金城, 罗佳. 利用COSMIC RO数据分析青藏高原平流层重力波活动特征[J]. 地球物理学报, 2016, 59(4):1199-1210)
[36]	LI Q Z, XU J Y, YUAN W, et al. Characteristics of mesospheric gravity waves over the southeastern Tibetan Plateau region[J]. J. Geophys. Res.:Space Phys., 2016, 121(9):9204-9221