华北地区冬小麦田水热、二氧化碳和甲烷湍流输送特征的实验研究

本文利用2012年4月30日至5月10日华北地区大气湍流实验资料,分析了冬小麦田下垫面温度、湿度、二氧化碳(CO_2)和甲烷(CH_4)的湍流统计和输送特征,利用涡旋相关法计算的CH_4通量值确定了松弛涡旋累积(REA)法计算CH_4通量的经验系数.结果表明,不稳定层结下,温度、湿度、CO_2和CH_4的归一化标准差随稳定度参数z/L的关系满足-1/3幂次关系.热量、水汽和CO_2水平方向的湍流输送和垂直方向的比值与稳定度参数z/L存在一定的相关关系,但CH_4没有类似特征.实验期间,感热通量数值较低,潜热通量较高;CO_2在夜间表现出微弱的向上输送,其余时段为向下输送,可以认为实验站所在地区...

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Main Authors: 葛红星, 张宏升, 罗帆, 蔡旭晖, 宋宇, 康凌, 霍庆
Other Authors: Ge, HX; Zhang, HS (reprint author), Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Beijing 100871, Peoples R China., 北京大学物理学院大气与海洋科学系,气候与海气实验室, 北京大学环境科学与工程学院环境科学系
Format: Journal/Newspaper
Language:Chinese
Published: 地球物理学报 2016
Subjects:
CO2
CH4
REA
Online Access:https://hdl.handle.net/20.500.11897/437457
https://doi.org/10.6038/cjg20160406
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record_format openpolar
spelling ftpekinguniv:oai:localhost:20.500.11897/437457 2023-05-15T16:39:30+02:00 华北地区冬小麦田水热、二氧化碳和甲烷湍流输送特征的实验研究 Turbulent characteristics of water, heat, carbon dioxide and methane transport over winter wheat fields of North China 葛红星 张宏升 罗帆 蔡旭晖 宋宇 康凌 霍庆 Ge, HX; Zhang, HS (reprint author), Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Beijing 100871, Peoples R China. 北京大学物理学院大气与海洋科学系,气候与海气实验室 北京大学环境科学与工程学院环境科学系 2016 https://hdl.handle.net/20.500.11897/437457 https://doi.org/10.6038/cjg20160406 zh chi 地球物理学报 地球物理学报.2016,59,(4),1235-1248. 1394840 http://hdl.handle.net/20.500.11897/437457 doi:10.6038/cjg20160406 WOS:000373864400006 CSCD SCI EI 知网 湍流输送 二氧化碳 甲烷 松弛涡旋累积(REA)法 华北地区 Turbulent transport CO2 CH4 REA North China RELAXED EDDY-ACCUMULATION VOSTOK ICE CORE FLUX MEASUREMENT COVARIANCE SYSTEM RICE FIELDS EMISSION ATMOSPHERE OXIDATION ISOPRENE Journal 2016 ftpekinguniv https://doi.org/20.500.11897/437457 https://doi.org/10.6038/cjg20160406 2021-08-01T10:50:09Z 本文利用2012年4月30日至5月10日华北地区大气湍流实验资料,分析了冬小麦田下垫面温度、湿度、二氧化碳(CO_2)和甲烷(CH_4)的湍流统计和输送特征,利用涡旋相关法计算的CH_4通量值确定了松弛涡旋累积(REA)法计算CH_4通量的经验系数.结果表明,不稳定层结下,温度、湿度、CO_2和CH_4的归一化标准差随稳定度参数z/L的关系满足-1/3幂次关系.热量、水汽和CO_2水平方向的湍流输送和垂直方向的比值与稳定度参数z/L存在一定的相关关系,但CH_4没有类似特征.实验期间,感热通量数值较低,潜热通量较高;CO_2在夜间表现出微弱的向上输送,其余时段为向下输送,可以认为实验站所在地区是碳汇;CH_4的湍流输送整体为向下输送,无明显的日变化规律,可以认为是CH_4汇.利用松弛涡旋累积法获取CO_2和CH_4通量的参数取值分别为0.61和0.30. Based on the turbulent observations during April 30 and May 10 2012, this work investigated statistical characteristics of atmospheric turbulent and water, heat, carbon dioxide (CO2) and methane (CH4) transport in North China. The empirical coefficient used to calculate the flux of CH4 in the Relaxed Eddy Accumulation (REA) method was simulated. The results show that in unstable conditions, the normalized standard deviations of temperature, humidity, CO2 and CH4 are related to z/L following the "-1/3 power law". The ratios between horizontal transport and vertical transport of heat, water vapor and CO2 are related to z/L, but CH4 has no similar relationship. Sensible heat flux is quite low while latent heat flux is relatively high. CO2 flux is slightly above zero during nighttime and below zero during daytime, indicating that the observed area is a carbon sink. CH4 flux is mainly below zero, indicating that the observed area is a methane sink. The values of the empirical coefficients used to calculate the flux of CO2 and CH4 in REA method are 0. 61 and 0. 30, respectively. 环保部公益性行业科研专项项目,国家自然科学基金 SCI(E) EI 中文核心期刊要目总览(PKU) 中国科技核心期刊(ISTIC) 中国科学引文数据库(CSCD) ge_star@163.com; hsdq@pku.edu.cn 4 1235-1248 59 Journal/Newspaper ice core Peking University Institutional Repository (PKU IR)
institution Open Polar
collection Peking University Institutional Repository (PKU IR)
op_collection_id ftpekinguniv
language Chinese
topic 湍流输送
二氧化碳
甲烷
松弛涡旋累积(REA)法
华北地区
Turbulent transport
CO2
CH4
REA
North China
RELAXED EDDY-ACCUMULATION
VOSTOK ICE CORE
FLUX MEASUREMENT
COVARIANCE SYSTEM
RICE FIELDS
EMISSION
ATMOSPHERE
OXIDATION
ISOPRENE
spellingShingle 湍流输送
二氧化碳
甲烷
松弛涡旋累积(REA)法
华北地区
Turbulent transport
CO2
CH4
REA
North China
RELAXED EDDY-ACCUMULATION
VOSTOK ICE CORE
FLUX MEASUREMENT
COVARIANCE SYSTEM
RICE FIELDS
EMISSION
ATMOSPHERE
OXIDATION
ISOPRENE
葛红星
张宏升
罗帆
蔡旭晖
宋宇
康凌
霍庆
华北地区冬小麦田水热、二氧化碳和甲烷湍流输送特征的实验研究
topic_facet 湍流输送
二氧化碳
甲烷
松弛涡旋累积(REA)法
华北地区
Turbulent transport
CO2
CH4
REA
North China
RELAXED EDDY-ACCUMULATION
VOSTOK ICE CORE
FLUX MEASUREMENT
COVARIANCE SYSTEM
RICE FIELDS
EMISSION
ATMOSPHERE
OXIDATION
ISOPRENE
description 本文利用2012年4月30日至5月10日华北地区大气湍流实验资料,分析了冬小麦田下垫面温度、湿度、二氧化碳(CO_2)和甲烷(CH_4)的湍流统计和输送特征,利用涡旋相关法计算的CH_4通量值确定了松弛涡旋累积(REA)法计算CH_4通量的经验系数.结果表明,不稳定层结下,温度、湿度、CO_2和CH_4的归一化标准差随稳定度参数z/L的关系满足-1/3幂次关系.热量、水汽和CO_2水平方向的湍流输送和垂直方向的比值与稳定度参数z/L存在一定的相关关系,但CH_4没有类似特征.实验期间,感热通量数值较低,潜热通量较高;CO_2在夜间表现出微弱的向上输送,其余时段为向下输送,可以认为实验站所在地区是碳汇;CH_4的湍流输送整体为向下输送,无明显的日变化规律,可以认为是CH_4汇.利用松弛涡旋累积法获取CO_2和CH_4通量的参数取值分别为0.61和0.30. Based on the turbulent observations during April 30 and May 10 2012, this work investigated statistical characteristics of atmospheric turbulent and water, heat, carbon dioxide (CO2) and methane (CH4) transport in North China. The empirical coefficient used to calculate the flux of CH4 in the Relaxed Eddy Accumulation (REA) method was simulated. The results show that in unstable conditions, the normalized standard deviations of temperature, humidity, CO2 and CH4 are related to z/L following the "-1/3 power law". The ratios between horizontal transport and vertical transport of heat, water vapor and CO2 are related to z/L, but CH4 has no similar relationship. Sensible heat flux is quite low while latent heat flux is relatively high. CO2 flux is slightly above zero during nighttime and below zero during daytime, indicating that the observed area is a carbon sink. CH4 flux is mainly below zero, indicating that the observed area is a methane sink. The values of the empirical coefficients used to calculate the flux of CO2 and CH4 in REA method are 0. 61 and 0. 30, respectively. 环保部公益性行业科研专项项目,国家自然科学基金 SCI(E) EI 中文核心期刊要目总览(PKU) 中国科技核心期刊(ISTIC) 中国科学引文数据库(CSCD) ge_star@163.com; hsdq@pku.edu.cn 4 1235-1248 59
author2 Ge, HX; Zhang, HS (reprint author), Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Beijing 100871, Peoples R China.
北京大学物理学院大气与海洋科学系,气候与海气实验室
北京大学环境科学与工程学院环境科学系
format Journal/Newspaper
author 葛红星
张宏升
罗帆
蔡旭晖
宋宇
康凌
霍庆
author_facet 葛红星
张宏升
罗帆
蔡旭晖
宋宇
康凌
霍庆
author_sort 葛红星
title 华北地区冬小麦田水热、二氧化碳和甲烷湍流输送特征的实验研究
title_short 华北地区冬小麦田水热、二氧化碳和甲烷湍流输送特征的实验研究
title_full 华北地区冬小麦田水热、二氧化碳和甲烷湍流输送特征的实验研究
title_fullStr 华北地区冬小麦田水热、二氧化碳和甲烷湍流输送特征的实验研究
title_full_unstemmed 华北地区冬小麦田水热、二氧化碳和甲烷湍流输送特征的实验研究
title_sort 华北地区冬小麦田水热、二氧化碳和甲烷湍流输送特征的实验研究
publisher 地球物理学报
publishDate 2016
url https://hdl.handle.net/20.500.11897/437457
https://doi.org/10.6038/cjg20160406
genre ice core
genre_facet ice core
op_source CSCD
SCI
EI
知网
op_relation 地球物理学报.2016,59,(4),1235-1248.
1394840
http://hdl.handle.net/20.500.11897/437457
doi:10.6038/cjg20160406
WOS:000373864400006
op_doi https://doi.org/20.500.11897/437457
https://doi.org/10.6038/cjg20160406
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