Continuity of daily temperature time series in the transition from conventional to automated stations for the Colombian coffee network
The transition from conventional weather stations (CWSs) to automated weather stations (AWSs) of the Colombian coffee network has required testing their performance and adjusting the temperature measurements to ensure the continuity of the historical CWS series. In this study, the mean (Tmean), mini...
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Published in: | Meteorological applications Vol. 29; no. 3 |
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01-05-2022
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Abstract | The transition from conventional weather stations (CWSs) to automated weather stations (AWSs) of the Colombian coffee network has required testing their performance and adjusting the temperature measurements to ensure the continuity of the historical CWS series. In this study, the mean (Tmean), minimum (Tmin), and maximum temperature (Tmax) measurements of CWS and AWS operating in parallel at 36 locations between 2014 and 2019 were compared, and the biases of the daily temperature differences (CWS − AWS), the agreement index (d), and the percentage of data within the allowed range (PR05) were calculated. The most consistent method for calculating Tmean and Tmax for CWS was selected for use on the AWS data. With the standard normal homogeneity test and with the metadata, we found that the series of temperature differences between CWS and AWS was not homogeneous, instrument failures and sensor changes being the main causes of the lack of homogeneity. The statistical analyses indicated that the AWS data need to be adjusted to be continuous with the CWS series. To correct the temperature bias, two approaches were applied: quantile mapping and the additive constant. The results suggest that the quantile mapping adjustments improve the average bias at all stations but do not necessarily bring the percentage to within ±0.5°C. In Tmin and Tmean, 12 AWSs can give continuity with the historical series of the CWS, and for the rest of the stations and variables, the series of the AWSs are independent of the CWSs.
The method to calculate the mean and maximum temperature in the automatic meteorological stations was selected to have a better concordance with the records of the conventional stations, and the automatic stations that give continuity to the historical series of the conventional network were specified. In the temperature variable, most of the automatic stations that operated in parallel with the conventional station have an independent series and will not give continuity to the historical series. |
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AbstractList | Abstract The transition from conventional weather stations (CWSs) to automated weather stations (AWSs) of the Colombian coffee network has required testing their performance and adjusting the temperature measurements to ensure the continuity of the historical CWS series. In this study, the mean (Tmean), minimum (Tmin), and maximum temperature (Tmax) measurements of CWS and AWS operating in parallel at 36 locations between 2014 and 2019 were compared, and the biases of the daily temperature differences (CWS − AWS), the agreement index (d), and the percentage of data within the allowed range (PR05) were calculated. The most consistent method for calculating Tmean and Tmax for CWS was selected for use on the AWS data. With the standard normal homogeneity test and with the metadata, we found that the series of temperature differences between CWS and AWS was not homogeneous, instrument failures and sensor changes being the main causes of the lack of homogeneity. The statistical analyses indicated that the AWS data need to be adjusted to be continuous with the CWS series. To correct the temperature bias, two approaches were applied: quantile mapping and the additive constant. The results suggest that the quantile mapping adjustments improve the average bias at all stations but do not necessarily bring the percentage to within ±0.5°C. In Tmin and Tmean, 12 AWSs can give continuity with the historical series of the CWS, and for the rest of the stations and variables, the series of the AWSs are independent of the CWSs. The transition from conventional weather stations (CWSs) to automated weather stations (AWSs) of the Colombian coffee network has required testing their performance and adjusting the temperature measurements to ensure the continuity of the historical CWS series. In this study, the mean (Tmean), minimum (Tmin), and maximum temperature (Tmax) measurements of CWS and AWS operating in parallel at 36 locations between 2014 and 2019 were compared, and the biases of the daily temperature differences (CWS − AWS), the agreement index (d), and the percentage of data within the allowed range (PR05) were calculated. The most consistent method for calculating Tmean and Tmax for CWS was selected for use on the AWS data. With the standard normal homogeneity test and with the metadata, we found that the series of temperature differences between CWS and AWS was not homogeneous, instrument failures and sensor changes being the main causes of the lack of homogeneity. The statistical analyses indicated that the AWS data need to be adjusted to be continuous with the CWS series. To correct the temperature bias, two approaches were applied: quantile mapping and the additive constant. The results suggest that the quantile mapping adjustments improve the average bias at all stations but do not necessarily bring the percentage to within ±0.5°C. In Tmin and Tmean, 12 AWSs can give continuity with the historical series of the CWS, and for the rest of the stations and variables, the series of the AWSs are independent of the CWSs. The transition from conventional weather stations (CWSs) to automated weather stations (AWSs) of the Colombian coffee network has required testing their performance and adjusting the temperature measurements to ensure the continuity of the historical CWS series. In this study, the mean (Tmean), minimum (Tmin), and maximum temperature (Tmax) measurements of CWS and AWS operating in parallel at 36 locations between 2014 and 2019 were compared, and the biases of the daily temperature differences (CWS − AWS), the agreement index (d), and the percentage of data within the allowed range (PR05) were calculated. The most consistent method for calculating Tmean and Tmax for CWS was selected for use on the AWS data. With the standard normal homogeneity test and with the metadata, we found that the series of temperature differences between CWS and AWS was not homogeneous, instrument failures and sensor changes being the main causes of the lack of homogeneity. The statistical analyses indicated that the AWS data need to be adjusted to be continuous with the CWS series. To correct the temperature bias, two approaches were applied: quantile mapping and the additive constant. The results suggest that the quantile mapping adjustments improve the average bias at all stations but do not necessarily bring the percentage to within ±0.5°C. In Tmin and Tmean, 12 AWSs can give continuity with the historical series of the CWS, and for the rest of the stations and variables, the series of the AWSs are independent of the CWSs. The method to calculate the mean and maximum temperature in the automatic meteorological stations was selected to have a better concordance with the records of the conventional stations, and the automatic stations that give continuity to the historical series of the conventional network were specified. In the temperature variable, most of the automatic stations that operated in parallel with the conventional station have an independent series and will not give continuity to the historical series. The transition from conventional weather stations (CWSs) to automated weather stations (AWSs) of the Colombian coffee network has required testing their performance and adjusting the temperature measurements to ensure the continuity of the historical CWS series. In this study, the mean ( T mean ), minimum ( T min ), and maximum temperature ( T max ) measurements of CWS and AWS operating in parallel at 36 locations between 2014 and 2019 were compared, and the biases of the daily temperature differences (CWS − AWS), the agreement index ( d ), and the percentage of data within the allowed range (PR05) were calculated. The most consistent method for calculating T mean and T max for CWS was selected for use on the AWS data. With the standard normal homogeneity test and with the metadata, we found that the series of temperature differences between CWS and AWS was not homogeneous, instrument failures and sensor changes being the main causes of the lack of homogeneity. The statistical analyses indicated that the AWS data need to be adjusted to be continuous with the CWS series. To correct the temperature bias, two approaches were applied: quantile mapping and the additive constant. The results suggest that the quantile mapping adjustments improve the average bias at all stations but do not necessarily bring the percentage to within ±0.5°C. In T min and T mean , 12 AWSs can give continuity with the historical series of the CWS, and for the rest of the stations and variables, the series of the AWSs are independent of the CWSs. |
Author | García López, Juan Carlos Sarmiento Herrera, Ninibeth Gibelli Imbachi Quinchua, Luis Carlos Ramírez Carabalí, Carolina |
Author_xml | – sequence: 1 givenname: Carolina orcidid: 0000-0001-8300-2623 surname: Ramírez Carabalí fullname: Ramírez Carabalí, Carolina email: carolina.ramirez@cafedecolombia.com, acl.cenicafe@cafedecolombia.com organization: National Center for Coffee Research, Cenicafé – sequence: 2 givenname: Ninibeth Gibelli orcidid: 0000-0002-7912-5708 surname: Sarmiento Herrera fullname: Sarmiento Herrera, Ninibeth Gibelli organization: National Center for Coffee Research, Cenicafé – sequence: 3 givenname: Luis Carlos orcidid: 0000-0002-4356-694X surname: Imbachi Quinchua fullname: Imbachi Quinchua, Luis Carlos organization: National Center for Coffee Research, Cenicafé – sequence: 4 givenname: Juan Carlos orcidid: 0000-0003-4861-9649 surname: García López fullname: García López, Juan Carlos organization: National Center for Coffee Research, Cenicafé |
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Cites_doi | 10.3929/ethz-b-000058274 10.1080/07055900.2015.1135784 10.5194/esd-4-219-2013 10.1002/met.271 10.1002/wcc.46 10.9734/JEAI/2018/40647 10.1175/1520-0426(1993)010≤0233:COMRAL>2.0.CO;2 10.1029/JC090iC05p08995 10.1002/joc.3370150403 10.1093/oso/9780195132717.001.0001 10.1175/2009JTECHA1241.1 10.5380/abclima.v12i1.30940 10.1175/2008JAMC1741.1 10.1175/JTECH1733.1 10.1175/2008JCLI2263.1 10.17951/b.2017.72.1.73 10.1029/2012JD017859 10.38141/10783/2018 10.1007/978-3-642-29172-2_24 10.5194/asr-13-163-2016 10.32614/RJ-2017-009 10.38141/10783/2014 10.1175/2010JAMC2376.1 10.1002/joc.5203 10.1002/joc.924 10.38141/10783/2017 10.1175/JTECH-D-15-0161.1 10.5351/KJAS.2012.25.6.977 10.1002/joc.3370060607 10.1002/joc.1602 10.1002/joc.5458 |
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Snippet | The transition from conventional weather stations (CWSs) to automated weather stations (AWSs) of the Colombian coffee network has required testing their... Abstract The transition from conventional weather stations (CWSs) to automated weather stations (AWSs) of the Colombian coffee network has required testing... |
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SubjectTerms | additive constant Additives automatic weather stations Automation Bias Coffee Continuity conventional weather station daily temperature Daily temperatures Homogeneity Mapping Mathematical analysis Maximum temperatures meteorological observation parallel observations quantile mapping Statistical analysis Statistical methods temperature bias Temperature differences Temperature gradients Temperature measurement Temperature requirements Weather Weather stations |
Title | Continuity of daily temperature time series in the transition from conventional to automated stations for the Colombian coffee network |
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