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Supplement of Added value of EURO-CORDEX high-resolution downscaling over the Iberian Peninsula revisited – Part 2: Max and min temperature

Digital.CSIC. Repositorio Institucional del CSIC
oai:digital.csic.es:10261/331478
Digital.CSIC. Repositorio Institucional del CSIC
  • Martins, João
  • Matos Soares, Pedro
  • Cardoso, Rita M.
  • Herrera, Sixto
  • Gutiérrez, José M.
Table S1. Regional models forced by the ERA-Interim reanalysis from the European Centre for Medium-Range Weather Forecasts, for the 1989-2008 period. Table S2. EURO-CORDEX Regional models driven by the CMIP5 GCMs. Also shown the approximate spatial resolution from each GCM taken from https://portal.enes.org/data/enes-model-data/cmip5/resolution. Figure S1. Maximum (left) and minimum (right) daily temperature distributions taken from the hindcast EURO-CORDEX RCMs and ERA-Interim reanalysis (1989-2008) for the Iberian Peninsula. Also shown the Iberian Gridded Dataset distribution for the same domain and period. All RCM data was previously interpolated into the IGD 0.1o regular resolution. As for Era-Interim, two PDFs are shown, one for the original resolution of the low-resolution and other interpolated into the IGD resolution. The dash point and the value written refers to either the 90th percentile for max temperature or the 10th percentile for min temperature of the observations for NGD on the original resolution (blue) and interpolated into the ERA-Interim resolution (red). The time periods are (a) Year, (b) DJF, (c) MAM, (d) JJA and (e) SON. Figure S2. Yearly and seasonal distribution added values (DAV) of the Iberian Peninsula, between the RCMs and the ERA-Interim reanalysis for the 1989-2008 period, taken from the Hindcast EURO-CORDEX simulations, with the IGD regular dataset as a reference for (a) maximum daily temperature, considering the whole PDF, (b) minimum daily temperature considering the whole PDF. (c) maximum daily temperature extremes, only considering the values above the observational 90th percentile from maximum temperatures and (d) minimum temperature extremes only considering the values below the observational 10th percentile from minimum temperatures. All model data were previously interpolated to 0.1o regular resolution from the observations. Figure S3. Maximum (left) and minimum (right) daily temperature distribution for the historical EURO-CORDEX RCMs driven by the CMIP5 GCMs, for the Iberian Peninsula, considering the 1971-2005 period, where all results were previously interpolated into the observational grid. The dash point and the value written refers to the 90th percentile of the observations for the maximum temperature and to the 10th percentile of the observations for the minimum temperature. (a) Year, (b) DJF, (c) MAM, (d) JJA and (e) SON. Figure S4. Maximum (left) and minimum (right) daily temperature distributions for the historical driving CMIP5 GCMs and IGD observations interpolated into each GCM resolution for the Iberian Peninsula, considering the 1971-2005 period. Also shown the PDF from the IGD observations at the original resolution. (a) Year, (b) DJF, (c) MAM, (d) JJA and (e) SON. Figure S5. Yearly and seasonal distribution added values (DAV) of the Iberian Peninsula, between the RCMs and the CMIP5 GCMs for the 1989-2008 period, taken from the Historical EURO-CORDEX simulations, with the IGD regular dataset as a reference for (a) maximum daily temperature, considering the whole PDF shown in the left panels of Figure S3, (b) minimum daily temperature considering the whole PDF shown in the right panels of Figure S3, (c) maximum daily temperature extremes, only considering the values above the observational 90th percentile from maximum temperatures and (d) minimum daily temperature extremes, only considering the values below the bservational 10th percentile from minimum temperatures. All model data were previously interpolated to 0.1o regular resolution from the observations. The thick blue lines separate the RCMs driven by different GCM., Peer reviewed
 
DOI: http://hdl.handle.net/10261/331478
Digital.CSIC. Repositorio Institucional del CSIC
oai:digital.csic.es:10261/331478

HANDLE: http://hdl.handle.net/10261/331478
Digital.CSIC. Repositorio Institucional del CSIC
oai:digital.csic.es:10261/331478
 
Ver en: http://hdl.handle.net/10261/331478
Digital.CSIC. Repositorio Institucional del CSIC
oai:digital.csic.es:10261/331478

Digital.CSIC. Repositorio Institucional del CSIC
oai:digital.csic.es:10261/331474
Set de datos (Dataset). 2022

SUPPLEMENT OF ADDED VALUE OF EURO-CORDEX HIGH-RESOLUTION DOWNSCALING OVER THE IBERIAN PENINSULA REVISITED - PART 1: PRECIPITATION

Digital.CSIC. Repositorio Institucional del CSIC
  • Martins, João
  • Matos Soares, Pedro
  • Cardoso, Rita M.
  • Herrera, Sixto
  • Gutiérrez, José M.
Table S1. Regional models driven by the ERA-Interim reanalysis from the European Centre for Medium-Range Weather Forecasts, for the 1989-2008 period. Table S2. EURO-CORDEX Regional models driven by the CMIP5 GCMs. Also shown the approximate spatial resolution from each GCM taken from https://portal.enes.org/data/enes-model-data/cmip5/resolution. Figure S1. Daily precipitation Intensity (left) and frequency (right) distributions taken from the hindcast EURO-CORDEX RCMs and ERA-Interim reanalysis (1989-2008) for the Iberian Peninsula. Also shown the Iberian Gridded Dataset distribution for the same domain and period. All RCM data was previously interpolated into the IGD 0.1o regular resolution. As for Era-Interim, two PDFs are shown, one for the original resolution of the low-resolution and other interpolated into the IGD resolution. The dash point and the value written refers to the 95th percentile of the observations for NGD on the original resolution (blue) and interpolated into the ERA-Interim resolution (red). The time periods are (a) Year, (b) DJF, (c) MAM, (d) JJA and (e) SON. Figure S2. Yearly and seasonal distribution added values (DAV) of the Iberian Peninsula, between the RCMs and the ERA-Interim reanalysis for the 1989-2008 period, taken from the Hindcast EURO-CORDEX simulations, with the NGD regular dataset as reference for (a) daily precipitation intensity, considering the whole PDF shown in the left panels of Figure S1, (b) daily precipitation frequency considering the whole PDF shown in the right panels of Figure S1, (c) daily precipitation intensity extremes, only considering the values above the observational 95th percentile shown in Figure S1 left side and (d) daily precipitation frequency extremes, only considering the values above the observational 95th percentile shown in the right side of Figure S1. All model data were previously interpolated to 0.1oregular resolution from the observations. Figure S3. Daily precipitation Intensity (left) and frequency (right) for the historical driving CMIP5 GCMs and EURO-CORDEX RCMs for the Iberian Peninsula, considering the 1971-2005 period, where all results were previously interpolated into the observational grid. The dash point and the value written refers to the 95th percentile of the bservations. (a) Year, (b) DJF, (c) MAM, (d) JJA and (e) SON. Figure S4. Daily precipitation Intensity (left) and frequency (right) for the historical driving CMIP5 GCMs and NGD observations interpolated into each GCM resolution for the Iberian Peninsula, considering the 1971-2005 period. Also shown the PDF from the NGD observations at the original resolution. (a) Year, (b) DJF, (c) MAM, (d) JJA and (e) SON. Figure S5. Yearly and seasonal distribution added values (DAV) of the Iberian Peninsula, between the RCMs and the CMIP5 GCMs for the 1989-2008 period, taken from the Historical EURO-CORDEX simulations, with the NGD regular dataset as reference for (a) daily precipitation intensity, considering the whole PDF shown in the left panels of Figure S3, (b) daily precipitation frequency considering the whole PDF shown in the right panels of Figure S3, (c) daily precipitation intensity extremes, only considering the values above the observational 95th percentile shown in Figure S3 left side and (d) daily precipitation frequency extremes, only considering the values above the observational 95th percentile shown in the right side of Figure S1. All model data were previously interpolated to 0.1o regular resolution from the observations. The thick blue lines separate the RCMs driven by different GCM., Peer reviewed




Digital.CSIC. Repositorio Institucional del CSIC
oai:digital.csic.es:10261/331478
Set de datos (Dataset). 2022

SUPPLEMENT OF ADDED VALUE OF EURO-CORDEX HIGH-RESOLUTION DOWNSCALING OVER THE IBERIAN PENINSULA REVISITED – PART 2: MAX AND MIN TEMPERATURE

Digital.CSIC. Repositorio Institucional del CSIC
  • Martins, João
  • Matos Soares, Pedro
  • Cardoso, Rita M.
  • Herrera, Sixto
  • Gutiérrez, José M.
Table S1. Regional models forced by the ERA-Interim reanalysis from the European Centre for Medium-Range Weather Forecasts, for the 1989-2008 period. Table S2. EURO-CORDEX Regional models driven by the CMIP5 GCMs. Also shown the approximate spatial resolution from each GCM taken from https://portal.enes.org/data/enes-model-data/cmip5/resolution. Figure S1. Maximum (left) and minimum (right) daily temperature distributions taken from the hindcast EURO-CORDEX RCMs and ERA-Interim reanalysis (1989-2008) for the Iberian Peninsula. Also shown the Iberian Gridded Dataset distribution for the same domain and period. All RCM data was previously interpolated into the IGD 0.1o regular resolution. As for Era-Interim, two PDFs are shown, one for the original resolution of the low-resolution and other interpolated into the IGD resolution. The dash point and the value written refers to either the 90th percentile for max temperature or the 10th percentile for min temperature of the observations for NGD on the original resolution (blue) and interpolated into the ERA-Interim resolution (red). The time periods are (a) Year, (b) DJF, (c) MAM, (d) JJA and (e) SON. Figure S2. Yearly and seasonal distribution added values (DAV) of the Iberian Peninsula, between the RCMs and the ERA-Interim reanalysis for the 1989-2008 period, taken from the Hindcast EURO-CORDEX simulations, with the IGD regular dataset as a reference for (a) maximum daily temperature, considering the whole PDF, (b) minimum daily temperature considering the whole PDF. (c) maximum daily temperature extremes, only considering the values above the observational 90th percentile from maximum temperatures and (d) minimum temperature extremes only considering the values below the observational 10th percentile from minimum temperatures. All model data were previously interpolated to 0.1o regular resolution from the observations. Figure S3. Maximum (left) and minimum (right) daily temperature distribution for the historical EURO-CORDEX RCMs driven by the CMIP5 GCMs, for the Iberian Peninsula, considering the 1971-2005 period, where all results were previously interpolated into the observational grid. The dash point and the value written refers to the 90th percentile of the observations for the maximum temperature and to the 10th percentile of the observations for the minimum temperature. (a) Year, (b) DJF, (c) MAM, (d) JJA and (e) SON. Figure S4. Maximum (left) and minimum (right) daily temperature distributions for the historical driving CMIP5 GCMs and IGD observations interpolated into each GCM resolution for the Iberian Peninsula, considering the 1971-2005 period. Also shown the PDF from the IGD observations at the original resolution. (a) Year, (b) DJF, (c) MAM, (d) JJA and (e) SON. Figure S5. Yearly and seasonal distribution added values (DAV) of the Iberian Peninsula, between the RCMs and the CMIP5 GCMs for the 1989-2008 period, taken from the Historical EURO-CORDEX simulations, with the IGD regular dataset as a reference for (a) maximum daily temperature, considering the whole PDF shown in the left panels of Figure S3, (b) minimum daily temperature considering the whole PDF shown in the right panels of Figure S3, (c) maximum daily temperature extremes, only considering the values above the observational 90th percentile from maximum temperatures and (d) minimum daily temperature extremes, only considering the values below the bservational 10th percentile from minimum temperatures. All model data were previously interpolated to 0.1o regular resolution from the observations. The thick blue lines separate the RCMs driven by different GCM., Peer reviewed




Digital.CSIC. Repositorio Institucional del CSIC
oai:digital.csic.es:10261/331474
Set de datos (Dataset). 2022

SUPPLEMENT OF ADDED VALUE OF EURO-CORDEX HIGH-RESOLUTION DOWNSCALING OVER THE IBERIAN PENINSULA REVISITED - PART 1: PRECIPITATION

Digital.CSIC. Repositorio Institucional del CSIC
  • Martins, João
  • Matos Soares, Pedro
  • Cardoso, Rita M.
  • Herrera, Sixto
  • Gutiérrez, José M.
Table S1. Regional models driven by the ERA-Interim reanalysis from the European Centre for Medium-Range Weather Forecasts, for the 1989-2008 period. Table S2. EURO-CORDEX Regional models driven by the CMIP5 GCMs. Also shown the approximate spatial resolution from each GCM taken from https://portal.enes.org/data/enes-model-data/cmip5/resolution. Figure S1. Daily precipitation Intensity (left) and frequency (right) distributions taken from the hindcast EURO-CORDEX RCMs and ERA-Interim reanalysis (1989-2008) for the Iberian Peninsula. Also shown the Iberian Gridded Dataset distribution for the same domain and period. All RCM data was previously interpolated into the IGD 0.1o regular resolution. As for Era-Interim, two PDFs are shown, one for the original resolution of the low-resolution and other interpolated into the IGD resolution. The dash point and the value written refers to the 95th percentile of the observations for NGD on the original resolution (blue) and interpolated into the ERA-Interim resolution (red). The time periods are (a) Year, (b) DJF, (c) MAM, (d) JJA and (e) SON. Figure S2. Yearly and seasonal distribution added values (DAV) of the Iberian Peninsula, between the RCMs and the ERA-Interim reanalysis for the 1989-2008 period, taken from the Hindcast EURO-CORDEX simulations, with the NGD regular dataset as reference for (a) daily precipitation intensity, considering the whole PDF shown in the left panels of Figure S1, (b) daily precipitation frequency considering the whole PDF shown in the right panels of Figure S1, (c) daily precipitation intensity extremes, only considering the values above the observational 95th percentile shown in Figure S1 left side and (d) daily precipitation frequency extremes, only considering the values above the observational 95th percentile shown in the right side of Figure S1. All model data were previously interpolated to 0.1oregular resolution from the observations. Figure S3. Daily precipitation Intensity (left) and frequency (right) for the historical driving CMIP5 GCMs and EURO-CORDEX RCMs for the Iberian Peninsula, considering the 1971-2005 period, where all results were previously interpolated into the observational grid. The dash point and the value written refers to the 95th percentile of the bservations. (a) Year, (b) DJF, (c) MAM, (d) JJA and (e) SON. Figure S4. Daily precipitation Intensity (left) and frequency (right) for the historical driving CMIP5 GCMs and NGD observations interpolated into each GCM resolution for the Iberian Peninsula, considering the 1971-2005 period. Also shown the PDF from the NGD observations at the original resolution. (a) Year, (b) DJF, (c) MAM, (d) JJA and (e) SON. Figure S5. Yearly and seasonal distribution added values (DAV) of the Iberian Peninsula, between the RCMs and the CMIP5 GCMs for the 1989-2008 period, taken from the Historical EURO-CORDEX simulations, with the NGD regular dataset as reference for (a) daily precipitation intensity, considering the whole PDF shown in the left panels of Figure S3, (b) daily precipitation frequency considering the whole PDF shown in the right panels of Figure S3, (c) daily precipitation intensity extremes, only considering the values above the observational 95th percentile shown in Figure S3 left side and (d) daily precipitation frequency extremes, only considering the values above the observational 95th percentile shown in the right side of Figure S1. All model data were previously interpolated to 0.1o regular resolution from the observations. The thick blue lines separate the RCMs driven by different GCM., Peer reviewed




Digital.CSIC. Repositorio Institucional del CSIC
oai:digital.csic.es:10261/331478
Set de datos (Dataset). 2022

SUPPLEMENT OF ADDED VALUE OF EURO-CORDEX HIGH-RESOLUTION DOWNSCALING OVER THE IBERIAN PENINSULA REVISITED – PART 2: MAX AND MIN TEMPERATURE

Digital.CSIC. Repositorio Institucional del CSIC
  • Martins, João
  • Matos Soares, Pedro
  • Cardoso, Rita M.
  • Herrera, Sixto
  • Gutiérrez, José M.
Table S1. Regional models forced by the ERA-Interim reanalysis from the European Centre for Medium-Range Weather Forecasts, for the 1989-2008 period. Table S2. EURO-CORDEX Regional models driven by the CMIP5 GCMs. Also shown the approximate spatial resolution from each GCM taken from https://portal.enes.org/data/enes-model-data/cmip5/resolution. Figure S1. Maximum (left) and minimum (right) daily temperature distributions taken from the hindcast EURO-CORDEX RCMs and ERA-Interim reanalysis (1989-2008) for the Iberian Peninsula. Also shown the Iberian Gridded Dataset distribution for the same domain and period. All RCM data was previously interpolated into the IGD 0.1o regular resolution. As for Era-Interim, two PDFs are shown, one for the original resolution of the low-resolution and other interpolated into the IGD resolution. The dash point and the value written refers to either the 90th percentile for max temperature or the 10th percentile for min temperature of the observations for NGD on the original resolution (blue) and interpolated into the ERA-Interim resolution (red). The time periods are (a) Year, (b) DJF, (c) MAM, (d) JJA and (e) SON. Figure S2. Yearly and seasonal distribution added values (DAV) of the Iberian Peninsula, between the RCMs and the ERA-Interim reanalysis for the 1989-2008 period, taken from the Hindcast EURO-CORDEX simulations, with the IGD regular dataset as a reference for (a) maximum daily temperature, considering the whole PDF, (b) minimum daily temperature considering the whole PDF. (c) maximum daily temperature extremes, only considering the values above the observational 90th percentile from maximum temperatures and (d) minimum temperature extremes only considering the values below the observational 10th percentile from minimum temperatures. All model data were previously interpolated to 0.1o regular resolution from the observations. Figure S3. Maximum (left) and minimum (right) daily temperature distribution for the historical EURO-CORDEX RCMs driven by the CMIP5 GCMs, for the Iberian Peninsula, considering the 1971-2005 period, where all results were previously interpolated into the observational grid. The dash point and the value written refers to the 90th percentile of the observations for the maximum temperature and to the 10th percentile of the observations for the minimum temperature. (a) Year, (b) DJF, (c) MAM, (d) JJA and (e) SON. Figure S4. Maximum (left) and minimum (right) daily temperature distributions for the historical driving CMIP5 GCMs and IGD observations interpolated into each GCM resolution for the Iberian Peninsula, considering the 1971-2005 period. Also shown the PDF from the IGD observations at the original resolution. (a) Year, (b) DJF, (c) MAM, (d) JJA and (e) SON. Figure S5. Yearly and seasonal distribution added values (DAV) of the Iberian Peninsula, between the RCMs and the CMIP5 GCMs for the 1989-2008 period, taken from the Historical EURO-CORDEX simulations, with the IGD regular dataset as a reference for (a) maximum daily temperature, considering the whole PDF shown in the left panels of Figure S3, (b) minimum daily temperature considering the whole PDF shown in the right panels of Figure S3, (c) maximum daily temperature extremes, only considering the values above the observational 90th percentile from maximum temperatures and (d) minimum daily temperature extremes, only considering the values below the bservational 10th percentile from minimum temperatures. All model data were previously interpolated to 0.1o regular resolution from the observations. The thick blue lines separate the RCMs driven by different GCM., Peer reviewed




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