Dantata Danlami, Sa’idu Idris, R. S. Thlakma, Golly Sammy Gwandum
{"title":"尼日利亚东北部HARMATTAN季节风速的时空变化","authors":"Dantata Danlami, Sa’idu Idris, R. S. Thlakma, Golly Sammy Gwandum","doi":"10.19184/GEOSI.V4I2.11474","DOIUrl":null,"url":null,"abstract":"Wind speed is the principal climatic element that drives the Marmaton season in West African sub region. It drives the season by conveying huge amount of dust across the Northeastern Nigeria. The presence of dust in the atmosphere brought by the Northeast trade winds during the Harmattan season plays a vital role in absorbing and scattering solar radiation. The study examines the spatial and temporal variations of wind speed in Northeastern Nigeria during the Harmattan season with the sole aim of ascertaining its variability, patterns and trends from1984 to 2014. Descriptive and statistics such as mean, standard deviation, coefficient of variation, and time series analysis with ArcGIS 10.3 was used in examine the temporal and spatial variations of wind speed from 1984–2014 in six synoptic stations of Northeastern Nigeria. The findings show that wind speed varied both temporally and spatially in the last three decades. The pattern of variations in the six synoptic stations shows rising trends within the study years. It was also found that latitude playing a crucial role in determining the speed of the wind in the study area and as the speed of the wind increases with increasing latitude. \nKeywords: Wind speed, Harmattan, Season, Northeast, Variation and ITD. \nReferences \nAdaramola,M.S.andOyewola,O. M. (2011). Wind Speed Distribution and Characteristics in Nigeria. Asian Research Publishing Network (ARPN). Journal of Engineering and Applied Sciences.ISSN 1819-6608.www.arpnjournals.com \nAmadi, S. O., Udo, S. O. and Ewona, I. O. (2014). Trends in Monthly Mean Minimum and Maximum Temperature Data over Nigeria for the Period 1950-2012. International Research Journal of Pure and Applied Physics, 2(4), 1-27. \nAyoade, J.O. (2004). Introduction to Climatology for the Tropics.2nd ed. Spectrum Books Limitted, Spectrum House Ring Road Ibadan, Nigeria. \nBalarabe, M., Abdallah, K., and Nawawi, M. (2015). Long- Term Trend and Seasonal Variability of Horizontal Visibility in Nigerian Troposphere.Journal of Atmosphere 6:1462-1486; doi:10.3390/atmos6101462. \nDahuwa, D., Promise, K. U., Umar, W., Bello, I. and Mohammed, R. (2018). Analysis of Wind Speed And Frequency InAzare North eastern Part of Nigeria. IOSR Journal of Applied Physics (IOSR-JAP) e-ISSN: 2278-4861.Volume 10, Issue 1 Ver. I. PP 09-17 www.iosrjournals.org DOI: 10.9790/4861-1001010917 www.iosrjournals.org \nDanlami, D., Gwari, M., Suleiman, S., and Bara, A. (2018). Temporal and Spatial variations of Groung Surface visibility during Harmattan Season in North-Eastern Nigeria.Ceylon Journal Science, 47(4), 337 – 346. DOI: http://doi.org/10.4038/cjs.v47i4.7551. \nDanlami, D. (2017). Spatio-Temporal Variations of Harmattan Season in Northeastern Nigeria.M.Sc. Dissertation (Not published) Submitted to the Department of Geography, Bayero University, Kano, Nigeria. \nDe Longueville, F., Hountondji, Y. C., Henry, S. and Ozer, P. (2010). What do we Know about the Effects of Desert Dust on Air Quality and Human Health in West Africa compared to other regions? Journal: Science of Total Environment \nFagbenle, R.L., Fasade, A.O., Amuludun A.K. andLala,P.O.( 1980). Wind power potentials of Nigeria. 12th Biennial conference of the West African Science Association, University of Ife, Nigeria. \nGetis, A., Getis, J., Bjelland, M. and Fellmann, J.D. (2011).Introduction to Geography. 13thed. The McGraw-Hill Companies, Inc., 1221 Avenue of the Americas, NY10020. \nKarabulut, M., Demirci, A. and Kora, F. (2012). Analysis of spatially distributed annual, seasonal and monthly temperatures in Istanbul from 1975 to 2006.World Applied Sciences Journal, 12(10), 1662-1675 \nOjosu, J.O. and Salawu, R.I. (1990).An evaluation of wind energy potential as a power generation source in Nigeria.Solar & Wind Technology.ELSEVIER.Volume 7, Issue 6, 1990, Pages 663-673 \nSchwanghart, W. and Schutt, B. (2007). Meteorological causes of Harmattan dust in West Africa. Journal of Science Direct Geomorphology. \nShuman, M. (2007) Evaluation of five GIS basedInterpolation techniques for estimating the Radonconcentration for unmeasured zip codes in thestate of Ohio, Master of Science Degree in Civil Engineering, University of Toledo, 28-29 Pp. \nWaewsak, J., Chancham, C., Landry, M. and Gagnon, Y (2011).An Analysis of Wind Speed Distribution at Thasala, Nakhon Si Thammarat, Thailand.Journal of Sustainable Energy & Environment 2 pp 51-55 \nWillmott, C., Robeson, S. and Philpot, W. (1985). Small- scale climate maps: A sensitivity analysisof some common assumptions associated withgrid-point interpolation and contouring. American Cartographer 12(1):5-16. \nCopyright (c) 2019 Geosfera Indonesia Journal and Department of Geography Education, University of Jember \n This work is licensed under a Creative Commons Attribution-Share A like 4.0 International License","PeriodicalId":33276,"journal":{"name":"Geosfera Indonesia","volume":" ","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2019-08-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":"{\"title\":\"THE SPATIO-TEMPORAL VARIATIONS OF WIND SPEED DURING HARMATTAN SEASON IN NORTHEASTERN NIGERIA\",\"authors\":\"Dantata Danlami, Sa’idu Idris, R. S. Thlakma, Golly Sammy Gwandum\",\"doi\":\"10.19184/GEOSI.V4I2.11474\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Wind speed is the principal climatic element that drives the Marmaton season in West African sub region. It drives the season by conveying huge amount of dust across the Northeastern Nigeria. The presence of dust in the atmosphere brought by the Northeast trade winds during the Harmattan season plays a vital role in absorbing and scattering solar radiation. The study examines the spatial and temporal variations of wind speed in Northeastern Nigeria during the Harmattan season with the sole aim of ascertaining its variability, patterns and trends from1984 to 2014. Descriptive and statistics such as mean, standard deviation, coefficient of variation, and time series analysis with ArcGIS 10.3 was used in examine the temporal and spatial variations of wind speed from 1984–2014 in six synoptic stations of Northeastern Nigeria. The findings show that wind speed varied both temporally and spatially in the last three decades. The pattern of variations in the six synoptic stations shows rising trends within the study years. It was also found that latitude playing a crucial role in determining the speed of the wind in the study area and as the speed of the wind increases with increasing latitude. \\nKeywords: Wind speed, Harmattan, Season, Northeast, Variation and ITD. \\nReferences \\nAdaramola,M.S.andOyewola,O. M. (2011). Wind Speed Distribution and Characteristics in Nigeria. Asian Research Publishing Network (ARPN). Journal of Engineering and Applied Sciences.ISSN 1819-6608.www.arpnjournals.com \\nAmadi, S. O., Udo, S. O. and Ewona, I. O. (2014). Trends in Monthly Mean Minimum and Maximum Temperature Data over Nigeria for the Period 1950-2012. International Research Journal of Pure and Applied Physics, 2(4), 1-27. \\nAyoade, J.O. (2004). Introduction to Climatology for the Tropics.2nd ed. Spectrum Books Limitted, Spectrum House Ring Road Ibadan, Nigeria. \\nBalarabe, M., Abdallah, K., and Nawawi, M. (2015). Long- Term Trend and Seasonal Variability of Horizontal Visibility in Nigerian Troposphere.Journal of Atmosphere 6:1462-1486; doi:10.3390/atmos6101462. \\nDahuwa, D., Promise, K. U., Umar, W., Bello, I. and Mohammed, R. (2018). Analysis of Wind Speed And Frequency InAzare North eastern Part of Nigeria. IOSR Journal of Applied Physics (IOSR-JAP) e-ISSN: 2278-4861.Volume 10, Issue 1 Ver. I. PP 09-17 www.iosrjournals.org DOI: 10.9790/4861-1001010917 www.iosrjournals.org \\nDanlami, D., Gwari, M., Suleiman, S., and Bara, A. (2018). Temporal and Spatial variations of Groung Surface visibility during Harmattan Season in North-Eastern Nigeria.Ceylon Journal Science, 47(4), 337 – 346. DOI: http://doi.org/10.4038/cjs.v47i4.7551. \\nDanlami, D. (2017). Spatio-Temporal Variations of Harmattan Season in Northeastern Nigeria.M.Sc. Dissertation (Not published) Submitted to the Department of Geography, Bayero University, Kano, Nigeria. \\nDe Longueville, F., Hountondji, Y. C., Henry, S. and Ozer, P. (2010). What do we Know about the Effects of Desert Dust on Air Quality and Human Health in West Africa compared to other regions? Journal: Science of Total Environment \\nFagbenle, R.L., Fasade, A.O., Amuludun A.K. andLala,P.O.( 1980). Wind power potentials of Nigeria. 12th Biennial conference of the West African Science Association, University of Ife, Nigeria. \\nGetis, A., Getis, J., Bjelland, M. and Fellmann, J.D. (2011).Introduction to Geography. 13thed. The McGraw-Hill Companies, Inc., 1221 Avenue of the Americas, NY10020. \\nKarabulut, M., Demirci, A. and Kora, F. (2012). Analysis of spatially distributed annual, seasonal and monthly temperatures in Istanbul from 1975 to 2006.World Applied Sciences Journal, 12(10), 1662-1675 \\nOjosu, J.O. and Salawu, R.I. (1990).An evaluation of wind energy potential as a power generation source in Nigeria.Solar & Wind Technology.ELSEVIER.Volume 7, Issue 6, 1990, Pages 663-673 \\nSchwanghart, W. and Schutt, B. (2007). Meteorological causes of Harmattan dust in West Africa. Journal of Science Direct Geomorphology. \\nShuman, M. (2007) Evaluation of five GIS basedInterpolation techniques for estimating the Radonconcentration for unmeasured zip codes in thestate of Ohio, Master of Science Degree in Civil Engineering, University of Toledo, 28-29 Pp. \\nWaewsak, J., Chancham, C., Landry, M. and Gagnon, Y (2011).An Analysis of Wind Speed Distribution at Thasala, Nakhon Si Thammarat, Thailand.Journal of Sustainable Energy & Environment 2 pp 51-55 \\nWillmott, C., Robeson, S. and Philpot, W. (1985). Small- scale climate maps: A sensitivity analysisof some common assumptions associated withgrid-point interpolation and contouring. 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引用次数: 2
摘要
风速是西非次区域Marmaton季节的主要气候因素。它通过在尼日利亚东北部输送大量灰尘来推动这个季节。Harmattan季节东北信风在大气中带来的灰尘在吸收和散射太阳辐射方面发挥着至关重要的作用。该研究考察了尼日利亚东北部Harmattan季节风速的空间和时间变化,唯一目的是确定1984年至2014年的变化、模式和趋势。利用ArcGIS 10.3的平均值、标准差、变异系数和时间序列分析等描述性和统计学方法,研究了尼日利亚东北部六个气象站1984年至2014年风速的时空变化。研究结果表明,在过去三十年中,风速在时间和空间上都有变化。六个天气站的变化模式在研究年份内呈上升趋势。研究还发现,纬度在决定研究区域的风速方面起着至关重要的作用,而且风速随着纬度的增加而增加。关键词:风速,Harmattan,季节,东北,变化和ITD。参考文献Adaramola,M。S.andOyewola,O.M.(2011)。尼日利亚的风速分布和特征。亚洲研究出版网络(ARPN)。工程与应用科学杂志。ISSN 1819-6608.www.arpnjournals.com Amadi,S.O.、Udo,S.O.和Ewona,I.O.(2014)。尼日利亚1950-2012年期间的月平均最低和最高温度数据趋势。国际纯粹与应用物理学研究杂志,2(4),1-27。Ayoade,J.O.(2004)。热带气候学导论第2版,Spectrum Books Limited,尼日利亚伊巴丹环城路Spectrum House。Balarabe,M.、Abdallah,K.和Nawawi,M.(2015)。尼日利亚对流层水平能见度的长期趋势和季节变化。《大气杂志》6:1462-1486;doi:10.3390/atmos610462。Dahwa,D.,Promise,K.U.,Umar,W.,Bello,I.和Mohammed,R.(2018)。尼日利亚东北部阿扎雷的风速和频率分析。IOSR应用物理学杂志(IOSR-JAP)e-ISSN:2278-861.第10卷第1期第一版PP 09-17 www.iosrjournals.org DOI:10.9790/4861-1001010917 www.iosrjaurnals.org Danlami,D.、Gwari,M.、Suleiman,S.和Bara,A.(2018)。尼日利亚东北部Harmattan季节Groung地表能见度的时空变化。《锡兰科学杂志》,47(4),337–346。DOI:http://doi.org/10.4038/cjs.v47i4.7551.Danlami,D.(2017)。尼日利亚东北部Harmattan季节的时空变化。硕士学位论文(未发表)提交给尼日利亚卡诺巴耶罗大学地理系。De Longueville,F.、Hountondji,Y.C.、Henry,S.和Ozer,P.(2010)。与其他地区相比,我们对西非沙漠沙尘对空气质量和人类健康的影响了解多少?《全面环境科学》,Fagbenle,R.L.,Fasade,A.O.,Amuludun A.K.和Lala,P。O.(1980)。尼日利亚的风能潜力。西非科学协会第12届双年度会议,尼日利亚伊夫大学。Getis,A.、Getis,J.、Bjelland,M.和Fellmann,J.D.(2011)。地理学导论。13。The McGraw-Hill Companies,股份有限公司,1221 Avenue of The Americas,NY10020。Karabulut,M.、Demirci,A.和Kora,F.(2012)。1975年至2006年伊斯坦布尔年、季节和月温度空间分布分析。《世界应用科学杂志》,12(10),1662-1675 Ojosu,J.O.和Salawu,R.I.(1990)。尼日利亚风能发电潜力评估。太阳能和风能技术。ELSEVIER。第7卷,1990年第6期,第663-673页,Schwanghart,W.和Schutt,B.(2007)。西非哈马坦沙尘的气象原因。科学杂志直接地貌学。Shuman,M.(2007)评估俄亥俄州未测量邮政编码的五种基于GIS的插值技术,土木工程理学硕士学位,托莱多大学,28-29页。Waewsak,J.,Chancham,C.,Landry,M.和Gagnon,Y(2011)。泰国呵叻府Thasala的风速分布分析。《可持续能源与环境杂志》,第51-55页,Willmott,C.、Robeson,S.和Philpot,W.(1985)。小尺度气候图:与网格点插值和轮廓相关的一些常见假设的敏感性分析。美国制图师12(1):5-16。版权所有(c)2019 Geosfera Indonesia Journal and Department of Geosfara Indonesia,University of Jember本作品根据知识共享署名共享类似4.0的国际许可证获得许可
THE SPATIO-TEMPORAL VARIATIONS OF WIND SPEED DURING HARMATTAN SEASON IN NORTHEASTERN NIGERIA
Wind speed is the principal climatic element that drives the Marmaton season in West African sub region. It drives the season by conveying huge amount of dust across the Northeastern Nigeria. The presence of dust in the atmosphere brought by the Northeast trade winds during the Harmattan season plays a vital role in absorbing and scattering solar radiation. The study examines the spatial and temporal variations of wind speed in Northeastern Nigeria during the Harmattan season with the sole aim of ascertaining its variability, patterns and trends from1984 to 2014. Descriptive and statistics such as mean, standard deviation, coefficient of variation, and time series analysis with ArcGIS 10.3 was used in examine the temporal and spatial variations of wind speed from 1984–2014 in six synoptic stations of Northeastern Nigeria. The findings show that wind speed varied both temporally and spatially in the last three decades. The pattern of variations in the six synoptic stations shows rising trends within the study years. It was also found that latitude playing a crucial role in determining the speed of the wind in the study area and as the speed of the wind increases with increasing latitude.
Keywords: Wind speed, Harmattan, Season, Northeast, Variation and ITD.
References
Adaramola,M.S.andOyewola,O. M. (2011). Wind Speed Distribution and Characteristics in Nigeria. Asian Research Publishing Network (ARPN). Journal of Engineering and Applied Sciences.ISSN 1819-6608.www.arpnjournals.com
Amadi, S. O., Udo, S. O. and Ewona, I. O. (2014). Trends in Monthly Mean Minimum and Maximum Temperature Data over Nigeria for the Period 1950-2012. International Research Journal of Pure and Applied Physics, 2(4), 1-27.
Ayoade, J.O. (2004). Introduction to Climatology for the Tropics.2nd ed. Spectrum Books Limitted, Spectrum House Ring Road Ibadan, Nigeria.
Balarabe, M., Abdallah, K., and Nawawi, M. (2015). Long- Term Trend and Seasonal Variability of Horizontal Visibility in Nigerian Troposphere.Journal of Atmosphere 6:1462-1486; doi:10.3390/atmos6101462.
Dahuwa, D., Promise, K. U., Umar, W., Bello, I. and Mohammed, R. (2018). Analysis of Wind Speed And Frequency InAzare North eastern Part of Nigeria. IOSR Journal of Applied Physics (IOSR-JAP) e-ISSN: 2278-4861.Volume 10, Issue 1 Ver. I. PP 09-17 www.iosrjournals.org DOI: 10.9790/4861-1001010917 www.iosrjournals.org
Danlami, D., Gwari, M., Suleiman, S., and Bara, A. (2018). Temporal and Spatial variations of Groung Surface visibility during Harmattan Season in North-Eastern Nigeria.Ceylon Journal Science, 47(4), 337 – 346. DOI: http://doi.org/10.4038/cjs.v47i4.7551.
Danlami, D. (2017). Spatio-Temporal Variations of Harmattan Season in Northeastern Nigeria.M.Sc. Dissertation (Not published) Submitted to the Department of Geography, Bayero University, Kano, Nigeria.
De Longueville, F., Hountondji, Y. C., Henry, S. and Ozer, P. (2010). What do we Know about the Effects of Desert Dust on Air Quality and Human Health in West Africa compared to other regions? Journal: Science of Total Environment
Fagbenle, R.L., Fasade, A.O., Amuludun A.K. andLala,P.O.( 1980). Wind power potentials of Nigeria. 12th Biennial conference of the West African Science Association, University of Ife, Nigeria.
Getis, A., Getis, J., Bjelland, M. and Fellmann, J.D. (2011).Introduction to Geography. 13thed. The McGraw-Hill Companies, Inc., 1221 Avenue of the Americas, NY10020.
Karabulut, M., Demirci, A. and Kora, F. (2012). Analysis of spatially distributed annual, seasonal and monthly temperatures in Istanbul from 1975 to 2006.World Applied Sciences Journal, 12(10), 1662-1675
Ojosu, J.O. and Salawu, R.I. (1990).An evaluation of wind energy potential as a power generation source in Nigeria.Solar & Wind Technology.ELSEVIER.Volume 7, Issue 6, 1990, Pages 663-673
Schwanghart, W. and Schutt, B. (2007). Meteorological causes of Harmattan dust in West Africa. Journal of Science Direct Geomorphology.
Shuman, M. (2007) Evaluation of five GIS basedInterpolation techniques for estimating the Radonconcentration for unmeasured zip codes in thestate of Ohio, Master of Science Degree in Civil Engineering, University of Toledo, 28-29 Pp.
Waewsak, J., Chancham, C., Landry, M. and Gagnon, Y (2011).An Analysis of Wind Speed Distribution at Thasala, Nakhon Si Thammarat, Thailand.Journal of Sustainable Energy & Environment 2 pp 51-55
Willmott, C., Robeson, S. and Philpot, W. (1985). Small- scale climate maps: A sensitivity analysisof some common assumptions associated withgrid-point interpolation and contouring. American Cartographer 12(1):5-16.
Copyright (c) 2019 Geosfera Indonesia Journal and Department of Geography Education, University of Jember
This work is licensed under a Creative Commons Attribution-Share A like 4.0 International License