{"title":"旱地气候变化动态与人类生物多样性响应","authors":"","doi":"10.24940/theijst/2021/v9/i8/st2108-014","DOIUrl":null,"url":null,"abstract":": The study has explored statistical and time series techniques that are used in the analysis of the data on conditional and specified activities of the atmosphere, ambient and sensible activities in Ado Ekiti, South West Nigeria. The plots of the atmospheric-ambient temperatures against sequential time series reveals an uneven pattern in temperature exponents or changes over the period covered, with behavioral trends with high relative wind speed resulting in most precipitations. It is visualized from the results that the ambient indices are with deviance of about ±4 (cid:3) (cid:4) compared to atmospheric data. Observations also shown from our comparisons that with atmospheric temperatures at about 33 (cid:3) (cid:4) ± 4 (cid:3) (cid:4) , saturated cloud resulting in precipitations were visible. Results show that, minus the tropical average atmospheric temperature which is 18 (cid:3) (cid:4) , maximum temperature (cid:9) (cid:10) (cid:11)(cid:12)(cid:13) determining features for precipitations are about 19.5 (cid:3) (cid:4) and 17.5 (cid:3) (cid:4) in May and June respectively, prevalent for specified days under study. Rarely on clear air days with about 33 (cid:3) (cid:4) ± 0 (cid:3) (cid:4) , possible precipitation was stratified or widespread when maximum temperature (cid:9) (cid:10) (cid:11)(cid:12)(cid:13) reaching about 15.0 (cid:3) (cid:4) and 17.0 (cid:3) (cid:4) justifying human biodiversity activities in the area of study. data and interpretations of the autistics of the ge dynamics continually interfaced by human biodiversity activities. analyses concerning different variables include sample days’ events and transect fitted graphs. This work estimated that ambient and atmospheric e significant to growing climate where precipitations as cloud cover are primary for reduction Our observatory study also confirms that conduction and heat exchange results in warm air and that equilibrium is usually reached when the solar radiation exceeds the terrestrial radiation for which fluctuating temperature exponents term good health of human beings depends on the continued stability and functioning between the weather system, the biosphere’s ecological system and The potential health consequences of climate change haveprovided human biodiversity with the basic and seasonal adjustment, climate, climate variability and climate change.","PeriodicalId":231256,"journal":{"name":"The International Journal of Science & Technoledge","volume":"19 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2021-08-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Climate Change Dynamics versus Human Biodiversity Responses in a Rainfall Upland Area\",\"authors\":\"\",\"doi\":\"10.24940/theijst/2021/v9/i8/st2108-014\",\"DOIUrl\":null,\"url\":null,\"abstract\":\": The study has explored statistical and time series techniques that are used in the analysis of the data on conditional and specified activities of the atmosphere, ambient and sensible activities in Ado Ekiti, South West Nigeria. The plots of the atmospheric-ambient temperatures against sequential time series reveals an uneven pattern in temperature exponents or changes over the period covered, with behavioral trends with high relative wind speed resulting in most precipitations. It is visualized from the results that the ambient indices are with deviance of about ±4 (cid:3) (cid:4) compared to atmospheric data. Observations also shown from our comparisons that with atmospheric temperatures at about 33 (cid:3) (cid:4) ± 4 (cid:3) (cid:4) , saturated cloud resulting in precipitations were visible. Results show that, minus the tropical average atmospheric temperature which is 18 (cid:3) (cid:4) , maximum temperature (cid:9) (cid:10) (cid:11)(cid:12)(cid:13) determining features for precipitations are about 19.5 (cid:3) (cid:4) and 17.5 (cid:3) (cid:4) in May and June respectively, prevalent for specified days under study. Rarely on clear air days with about 33 (cid:3) (cid:4) ± 0 (cid:3) (cid:4) , possible precipitation was stratified or widespread when maximum temperature (cid:9) (cid:10) (cid:11)(cid:12)(cid:13) reaching about 15.0 (cid:3) (cid:4) and 17.0 (cid:3) (cid:4) justifying human biodiversity activities in the area of study. data and interpretations of the autistics of the ge dynamics continually interfaced by human biodiversity activities. analyses concerning different variables include sample days’ events and transect fitted graphs. This work estimated that ambient and atmospheric e significant to growing climate where precipitations as cloud cover are primary for reduction Our observatory study also confirms that conduction and heat exchange results in warm air and that equilibrium is usually reached when the solar radiation exceeds the terrestrial radiation for which fluctuating temperature exponents term good health of human beings depends on the continued stability and functioning between the weather system, the biosphere’s ecological system and The potential health consequences of climate change haveprovided human biodiversity with the basic and seasonal adjustment, climate, climate variability and climate change.\",\"PeriodicalId\":231256,\"journal\":{\"name\":\"The International Journal of Science & Technoledge\",\"volume\":\"19 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2021-08-31\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"The International Journal of Science & Technoledge\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.24940/theijst/2021/v9/i8/st2108-014\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"The International Journal of Science & Technoledge","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.24940/theijst/2021/v9/i8/st2108-014","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Climate Change Dynamics versus Human Biodiversity Responses in a Rainfall Upland Area
: The study has explored statistical and time series techniques that are used in the analysis of the data on conditional and specified activities of the atmosphere, ambient and sensible activities in Ado Ekiti, South West Nigeria. The plots of the atmospheric-ambient temperatures against sequential time series reveals an uneven pattern in temperature exponents or changes over the period covered, with behavioral trends with high relative wind speed resulting in most precipitations. It is visualized from the results that the ambient indices are with deviance of about ±4 (cid:3) (cid:4) compared to atmospheric data. Observations also shown from our comparisons that with atmospheric temperatures at about 33 (cid:3) (cid:4) ± 4 (cid:3) (cid:4) , saturated cloud resulting in precipitations were visible. Results show that, minus the tropical average atmospheric temperature which is 18 (cid:3) (cid:4) , maximum temperature (cid:9) (cid:10) (cid:11)(cid:12)(cid:13) determining features for precipitations are about 19.5 (cid:3) (cid:4) and 17.5 (cid:3) (cid:4) in May and June respectively, prevalent for specified days under study. Rarely on clear air days with about 33 (cid:3) (cid:4) ± 0 (cid:3) (cid:4) , possible precipitation was stratified or widespread when maximum temperature (cid:9) (cid:10) (cid:11)(cid:12)(cid:13) reaching about 15.0 (cid:3) (cid:4) and 17.0 (cid:3) (cid:4) justifying human biodiversity activities in the area of study. data and interpretations of the autistics of the ge dynamics continually interfaced by human biodiversity activities. analyses concerning different variables include sample days’ events and transect fitted graphs. This work estimated that ambient and atmospheric e significant to growing climate where precipitations as cloud cover are primary for reduction Our observatory study also confirms that conduction and heat exchange results in warm air and that equilibrium is usually reached when the solar radiation exceeds the terrestrial radiation for which fluctuating temperature exponents term good health of human beings depends on the continued stability and functioning between the weather system, the biosphere’s ecological system and The potential health consequences of climate change haveprovided human biodiversity with the basic and seasonal adjustment, climate, climate variability and climate change.