Research on temporal and spatial differences of atmospheric water vapor and its driving factors over Liupan Mountain area

doi:10.11755/j.issn.1006-7639(2024)-03-0376

Journal of Arid Meteorology ›› 2024, Vol. 42 ›› Issue (3): 376-384.DOI: 10.11755/j.issn.1006-7639(2024)-03-0376

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Research on temporal and spatial differences of atmospheric water vapor and its driving factors over Liupan Mountain area

DENG Peiyun¹^,²^,³(), CHANG Zhuolin¹^,²^,³(), HE Jia¹^,²^,³, YANG Meng⁴, CHEN Deyuan⁵, LIN Tong¹^,²^,³, MU Jianhua¹^,²^,³, DAI Yanbo¹^,²^,³

1. Liupanshan Atmospheric Science Field Observation and Research Station in Ningxia Hui Autonomous Region， Yinchuan 750002， China
2. Key Laboratory of Monitoring， Warning and Risk Management of Characteristic Agrometeorological Disasters in Arid Regions， China Meteorological Administration， Yinchuan 750002， China
3. Ningxia Key Laboratory of Meteorological Disaster Prevention and Mitigation， Yinchuan 750002， China
4. Yibin Meteorological Bureau of Sichuan Province， Yibin 644000， Sichuan， China
5. Lanzhou Central Meteorological Observatory， Lanzhou 730020， China

Received:2022-10-31 Revised:2023-01-04 Online:2024-06-30 Published:2024-07-11

六盘山地区大气水汽的时空差异与驱动因子分析

邓佩云¹^,²^,³(), 常倬林¹^,²^,³(), 何佳¹^,²^,³, 杨萌⁴, 陈得圆⁵, 林彤¹^,²^,³, 穆建华¹^,²^,³, 戴言博¹^,²^,³

1.六盘山大气科学宁夏回族自治区野外科学观测研究站，宁夏银川 750002
2.中国气象局旱区特色农业气象灾害监测预警与风险管理重点实验室，宁夏银川 750002
3.宁夏气象防灾减灾重点实验室，宁夏银川 750002
4.四川省宜宾市气象局，四川宜宾 644000
5.兰州中心气象台，甘肃兰州 730020

通讯作者: 常倬林（1981—），女，山西文水人，正高级工程师，主要从事大气物理与人工影响天气方面研究。E-mail:changzhl05@126.com。
作者简介:邓佩云（1993—），女，宁夏固原人，工程师，主要从事大气物理与人工影响天气方面研究。E-mail:734785297@qq.com。
基金资助:
国家自然科学基金区域创新发展联合基金项目(U22A20577);宁夏回族自治区重点研发计划项目重点项目(2022BEG02010);宁夏回族自治区科技创新团队“宁夏智能数字预报技术研究与应用”项目(2024CXTD006);中国气象局旱区特色农业气象灾害监测预警与风险管理重点实验室开放研究项目(CAMF-202306);中国气象局旱区特色农业气象灾害监测预警与风险管理重点实验室开放研究项目(CAMF-201814);中国气象局创新发展专项(CXFZ2022J035)

Abstract

Abstract:

In order to effectively develop the cloud water resources in the Liupan Mountain area and improve the scientificity of artificial precipitation enhancement, it is necessary to grasp the spatial and temporal distribution characteristics of atmospheric water vapor in the region and its causes. In this paper, the precipitation observation data of national basic meteorological stations in the Liupan Mountain area from 1989 to 2018 and the Fifth Generation Atmospheric Reanalysis Data (ERA5) of European Centre for Medium-Range Weather Forecasts (ECMWF) during the same period are used to analyze the spatial and temporal changes of atmospheric water vapor elements such as precipitable water, specific humidity, relative humidity and water vapor flux in this area. The reasons for the difference of water vapor conditions and precipitation in different areas of the Liupan Mountain area are analyzed from the aspects of water vapor transport, terrain effect and influence of buoyancy frequency. The results show that the water vapor conditions over the top and the east slope of the Liupan Mountain are better than those over the west slope in most of the year. The large value areas are mainly concentrated near the main peak of the Liupan Mountain, and water vapor condition has obvious seasonal variation characteristics. Over the eastern slope of the Liupan Mountain, the dynamic field of 500 hPa divergence and 700 hPa convergence caused by the uplift of the terrain is the most obvious in summer and the weakest in winter. The buoyancy frequency is the highest in winter and the lowest in summer. The higher buoyancy frequency and steeper terrain on the eastern slope make the gravity wave effect more obvious, resulting in more favorable vertical upward diffusion conditions and greater precipitation potential.

Key words: the Liupan Mountain area, atmospheric precipitable water, water vapor condition, orographic lifting, impact factor

摘要：

为有效开发六盘山地区空中云水资源，提高人工增雨的科学性，需掌握该区域大气水汽的时空分布特征及其原因。利用1989—2018年六盘山地区国家基本站降水观测资料和同期欧洲中期天气预报中心（European Centre for Medium-Range Weather Forecasts，ECMWF）第五代大气再分析资料（ERA5），分析该区域大气可降水量、比湿、相对湿度、水汽通量等大气水汽要素的时空变化，并从水汽输送、地形作用、浮力频率的影响等方面分析六盘山不同地区水汽条件及降水差异的原因。结果表明：一年中绝大多数时间六盘山山顶及东坡大气水汽条件均优于西坡，大值区主要集中在六盘山系主峰附近，并具有明显的季节变化特征。六盘山东坡，受地形抬升作用引起500 hPa辐散、700 hPa辐合的动力场，在夏季最明显，冬季最弱；浮力频率冬季最高，夏季最低；东坡更高的浮力频率及更陡峭的地形，使重力波效应更为明显，具备更有利的垂直上升扩散条件及更大的降水潜力。

关键词: 六盘山, 大气可降水量, 水汽条件, 地形抬升, 影响因子

CLC Number:

P481

DENG Peiyun, CHANG Zhuolin, HE Jia, YANG Meng, CHEN Deyuan, LIN Tong, MU Jianhua, DAI Yanbo. Research on temporal and spatial differences of atmospheric water vapor and its driving factors over Liupan Mountain area[J]. Journal of Arid Meteorology, 2024, 42(3): 376-384.

邓佩云, 常倬林, 何佳, 杨萌, 陈得圆, 林彤, 穆建华, 戴言博. 六盘山地区大气水汽的时空差异与驱动因子分析[J]. 干旱气象, 2024, 42(3): 376-384.

Figures/Tables 11

References 32

[1]	常倬林, 崔洋, 2022. 六盘山地区大气水汽资源特征及开发潜力分析[J]. 宁夏农林科技, 63(4): 53-56.
[2]	常倬林, 崔洋, 张武, 等, 2015. 基于CERES的宁夏空中云水资源特征及其增雨潜力研究[J]. 干旱区地理, 38(6): 1 112-1 120.
[3]	陈国华, 2013. 基于统计降尺度的中国地面气温精细化预报方法研究[D]. 南京: 南京信息工程大学.
[4]	陈海波, 杨建玲, 丁建军, 等, 2013. 宁夏水汽输送气候特征[J]. 干旱气象, 31(3): 491-496. DOI
[5]	陈炜, 李跃清, 2018. 对流层重力波的主要研究进展[J]. 干旱气象, 36(5): 717-724. DOI
[6]	邓佩云, 桑建人, 杨萌, 等, 2021. 近30年六盘山东与西坡降水及空中水汽条件差异特征分析[J]. 气象科技, 49(1): 77-85.
[7]	方文维, 朱紫云, 林日新, 2019. 我国大气可降水量变化特征分析[J]. 海峡科学, (7): 19-24.
[8]	冯建民, 2012. 宁夏天气预报手册[M]. 北京: 气象出版社.
[9]	韩雪云, 赵丽, 张倩, 等, 2019. 西北干旱区极端高温时空变化特征分析[J]. 沙漠与绿洲气象, 13(4): 17-23.
[10]	胡振菊, 黎璐, 黄小玉, 等, 2022. 一次典型东风波极端暴雨的中尺度特征及地形影响分析[J]. 干旱气象, 40(1): 73-83. DOI
[11]	黄露, 范广洲, 2018. 影响青藏高原大气可降水量的因素及其变化特征[J]. 气象科技, 46(6): 1 172-1 179.
[12]	李芳芳, 2019. 东亚地区重力波动量通量谱分布特征[D]. 成都: 成都信息工程大学.
[13]	廖菲, 洪延超, 郑国光, 2006. 影响云和降水的动力、热力与微物理因素的研究概述[J]. 气象, 32(11): 3-11.
[14]	刘珂, 姜大膀, 2014. 中国夏季和冬季极端干旱年代际变化及成因分析[J]. 大气科学, 38(2): 309-321.
[15]	刘炜, 赵艳丽, 冯晓晶, 2021. 内蒙古地区夏季旱涝急转环流异常特征及其预测[J]. 干旱气象, 39(2) : 203-214.
[16]	刘宇佳, 满文敏, 周天军, 等, 2023. 中国东部地区大气水汽稳定同位素的影响因子追踪研究[J]. 大气科学, 47(3): 616-630.
[17]	唐国瑛, 李丰全, 王莺, 等, 2022. 青藏高原东北边缘地带2017—2020年地闪时空分布特征[J]. 干旱气象, 40(5): 849-856. DOI
[18]	王婉, 雷恒池, 聂皓浩, 等, 2021. 基于机载微波辐射计探测大气水汽通道饱和问题研究[J]. 气象学报, 79(3): 509-520.
[19]	王莺, 张强, 王劲松, 等, 2022. 21世纪以来干旱研究的若干新进展与展望[J]. 干旱气象, 40(4): 549-566. DOI
[20]	徐祥德, 陶诗言, 王继志, 等, 2002. 青藏高原—季风水汽输送“大三角扇型”影响域特征与中国区域旱涝异常的关系[J]. 气象学报, 60(3): 257-266.
[21]	薛亮, 袁淑杰, 王劲松, 2023. 我国不同区域气象干旱成因研究进展与展望[J]. 干旱气象, 41(1):1-13. DOI
[22]	薛媛, 薛晓萍, 2022. 极端降水与干旱同步频发的研究进展[J]. 海洋气象学报, 42(1): 61-73.
[23]	尹宪志, 王毅荣, 徐文君, 等, 2020. 祁连山空中云水资源开发潜力研究新进展[J]. 沙漠与绿洲气象, 14(6):134-140.
[24]	张继波, 薛晓萍, 李楠, 等, 2019. 干旱胁迫对冬小麦水分关键期的生理特性和物质生产影响[J]. 沙漠与绿洲气象, 13(3): 124-130.
[25]	张沛, 姚展予, 贾烁, 等, 2020. 六盘山地区空中水资源特征及水凝物降水效率研究[J]. 大气科学, 44(2): 421-434.
[26]	张强, 杨金虎, 马鹏里, 等, 2023. 西北地区气候暖湿化增强东扩特征及其形成机制与重要环境影响[J]. 干旱气象, 41(3): 351-358. DOI
[27]	赵美, 李永, 张军, 等, 2011. 高空700 hPa规定层比湿与地面降水关系分析[C]// “推进气象科技创新,提高防灾减灾和应对气候变化能力”——江苏省气象学会第七届学术交流会论文集, 苏州.
[28]	庄晓翠, 李博渊, 赵江伟, 等, 2022. 天山南坡暖季暴雨过程的水汽来源及输送特征[J]. 干旱气象, 40(1): 30-40. DOI
[29]	KIRSHBAUM D J, DURRAN D R, 2004. Factors governing cellular convection in orographic precipitation[J]. Journal of the Atmospheric Sciences, 61(6): 682-698.
[30]	MORALES A, POSSELT D J, MORRISON H, et al, 2019. Assessing the influence of microphysical and environmental parameter perturbations on orographic precipitation[J]. Journal of the Atmospheric Sciences, 76(5): 1 373-1 395.
[31]	REINKING R F, SNIDER J B, COEN J L, 2000. Influences of storm-embedded orographic gravity waves on cloud liquid water and precipitation[J]. Journal of Applied Meteorology, 39(6): 733-759.
[32]	ROCKEN C, VAN HOVE T, JOHNSON J, et al, 1995. GPS/STORM-GPS sensing of atmospheric water vapor for meteorology[J]. Journal of Atmospheric and Oceanic Technology, 12(3): 468-478.

季节	西吉	隆德	六盘山	泾源	彭阳	固原	平均
春季	73.06	87.78	108.49	122.77	57.82	77.40	87.89
夏季	226.28	285.71	340.02	355.04	155.89	258.24	270.20
秋季	95.57	118.92	151.10	155.89	81.80	100.61	117.32
冬季	9.69	15.86	25.56	19.42	8.26	11.84	15.11

季节	西吉	隆德	六盘山	泾源	彭阳	固原	平均
春季	73.06	87.78	108.49	122.77	57.82	77.40	87.89
夏季	226.28	285.71	340.02	355.04	155.89	258.24	270.20
秋季	95.57	118.92	151.10	155.89	81.80	100.61	117.32
冬季	9.69	15.86	25.56	19.42	8.26	11.84	15.11

季节	西吉	隆德	六盘山	泾源	彭阳	固原
春季	9.01	9.24	9.21	9.41	10.11	9.19
夏季	21.54	21.88	21.90	22.18	24.33	22.25
秋季	11.35	11.55	11.53	11.73	12.87	11.65
冬季	3.93	4.05	4.02	4.09	4.46	4.03

季节	西吉	隆德	六盘山	泾源	彭阳	固原
春季	9.01	9.24	9.21	9.41	10.11	9.19
夏季	21.54	21.88	21.90	22.18	24.33	22.25
秋季	11.35	11.55	11.53	11.73	12.87	11.65
冬季	3.93	4.05	4.02	4.09	4.46	4.03

季节	西吉	隆德	六盘山	泾源	彭阳	固原
春季	3.14	3.27	3.25	3.36	3.09	3.05
夏季	7.47	7.70	7.68	7.82	7.32	7.33
秋季	3.88	3.98	3.97	4.07	3.76	3.77
冬季	1.31	1.36	1.35	1.38	1.28	1.27

Research on temporal and spatial differences of atmospheric water vapor and its driving factors over Liupan Mountain area

六盘山地区大气水汽的时空差异与驱动因子分析

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Figures/Tables 11

References 32

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季节	西吉	隆德	六盘山	泾源	彭阳	固原
春季	53.84	55.56	55.57	57.11	53.23	52.20
夏季	65.36	67.77	67.99	69.34	64.56	64.18
秋季	59.72	60.86	61.04	62.30	57.84	57.76
冬季	49.68	50.64	50.51	51.36	47.97	48.07

季节	西吉	隆德	六盘山	泾源	彭阳	固原
春季	0.52	0.54	0.56	0.55	0.67	0.65
夏季	1.69	1.88	1.84	1.88	1.51	1.54
秋季	0.85	0.99	1.00	1.03	0.99	0.96
冬季	0.49	0.51	0.53	0.51	0.60	0.59

季节	区域	大气可降水量/mm	700 hPa比湿/（g·kg^-1）	700 hPa相对湿度/%	700 hPa水汽通量/[g·（s·hPa·cm）^-1]
春季	东坡	9.57	3.16	54.18	0.62
	西坡	9.12	3.20	54.70	0.53
	六盘山地区	9.36	3.19	54.59	0.58
夏季	东坡	22.92	7.49	66.03	1.64
	西坡	21.71	7.58	66.56	1.78
	六盘山地区	22.35	7.55	66.53	1.72
秋季	东坡	12.08	3.86	59.30	0.99
	西坡	11.45	3.93	60.29	0.92
	六盘山地区	11.78	3.90	59.92	0.97
冬季	东坡	4.19	1.31	49.13	0.57
	西坡	3.99	1.33	50.16	0.50
	六盘山地区	4.10	1.32	49.70	0.54

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