Literature DB >> 32345985

A multidecadal assessment of climate indices over Europe.

Fernando Domínguez-Castro1,2, Fergus Reig3, Sergio M Vicente-Serrano3, Enric Aguilar4, Dhais Peña-Angulo3, Iván Noguera3, Jesús Revuelto3, Gerard van der Schrier5, Ahmed M El Kenawy6,7.   

Abstract

Monitoring and management of several environmental and socioeconomic sectors require climate data that can be summarized using a set of standard and meaningful climate metrics. This study describes a newly developed gridded dataset for the whole of Europe, which employed a set of 125 climate indices spanning different periods based on data availability, but mainly 1950-2017 and 1979-2017. This dataset comprehensively summarizes climate variability in Europe for a wide range of climate variables and conditions, including air temperature, precipitation, biometeorology, aridity, continentality, drought, amongst others. Climate indices were computed at different temporal scales (i.e. monthly, seasonal and annual) and mapped at a grid interval of 0.25°. We intend to update these indices on an annual basis. This dataset is freely available to research and end-user communities.

Entities:  

Year:  2020        PMID: 32345985      PMCID: PMC7188899          DOI: 10.1038/s41597-020-0464-0

Source DB:  PubMed          Journal:  Sci Data        ISSN: 2052-4463            Impact factor:   6.444


Background & Summary

Climate processes are complex and therefore hard to monitor and quantify.This is mainly due to the different environmental and socioeconomic impacts of climate, which pose further challenges to climate quantification and assessment[1-3]. Although climate observations usually correspond to quantitative variables with a comprehensible physical meaning, the environmental, societal and economic impacts, including a number of sectors, usually depend on specific climate conditions or event characteristics[4-7]. For example, the cumulative climate conditions over long periods, the extreme values recorded over a period, the frequency of days with specific characteristics, the frequency of events above or below specific thresholds; amongst others, could have a direct influence on environmental and socioeconomic systems[8-11]. In the same context, monitoring and assessing the impact of climate is a complicated process, given that conditions that trigger specific impacts are often a result of interactions between different climate covariates. For example, bioclimatic conditions that strongly determine human health and comfort depend on a wide range of climate variables, such as air temperature, relative humidity, wind speed, etc.[12,13]. Similarly, while drought severity is mainly controlled by precipitation, other climate variables (e.g. atmospheric evaporative demand, potential evaporation) could contribute significantly to drought dynamics[14-16]. Within this context, much effort has been made to develop synthetic climate indices, which can be employed to determine climate impacts on different natural systems and socioeconomic sectors[17-21]. These indices are also useful for providing a comprehensive assessment of climate variability and change processes under current and future climate change scenarios[22-25]. The joint Ccl/WCRP/JCOMM Expert Team on Climate Change Detection and Indices (ETCCDI)[26] developed an array of standard climate indices, which have widely been used to determine recent trends in climate conditions, with a particular focus on precipitation and temperature metrics. These indices have been widely used over different world regions such as Brazil[27], China[28,29], Africa[30,31], the Mediterranean[32,33], Indonesia[34], North America[35], central America[36], central Asia[37], amongst others. In addition, these indices have also been analyzed to assess the consequences of projections for future climate change scenarios. For example, Aerenson et al.[38] have recently analyzed a suite of climate indices based on daily precipitation and temperature projections at the global scale, with the aim of determining possible future changes under 1.5 °C and 2 °C warming scenarios. Their study indicated that temperature indices are likely to witness significant changes in the future. On the other hand, the behavior of precipitation indices is more complex and different scenarios may cause different changes in the intensity of precipitation. Other studies (e.g. Dong et al.[39]) employed climate indices to verify that the observed warming trends in Asia in the past six decades were inconsistent with the natural variability of the climate system, but agreed with climate responses to external forcing, as simulated by the models. The availability of long-term, high spatial resolution and updated climate indices could be promising for the research community through a multidecadal assessment of climate change processes and their impacts. This climate information could also be useful for a wide variety of environmental and socioeconomic sectors (e.g. land and agricultural management, climate-based health impacts, insurance plans associated with weather extremes, etc). Currently, some climate indices datasets have been developed[35,40], mostly with the purpose of analyzing trends in climate conditions, focusing more on extreme meteorological events[41,42]. There are some worldwide updated climate indices dataset, such as i) DegDays_0p25_1970_2018[43], which provides indices summarizing monthly and annual cooling and heating degree –days at the global scale, ii) GHCNDEX[41], which includes a wide range of the ETCCDI indices calculated at the global scale, and iii) the global drought monitoring dataset based on the standardized precipitation evapotranspiration index[44]. Nevertheless, in Europe, there is no updated dataset of a wide variety of climate indices that can be useful not only for climate analysis, but also for a broad sectorial impact assessment. For this reason, the objective of this study is to provide an updated gridded dataset of a large variety of climate indices that summarize the temporal and spatial variability of climate in Europe during the past seven decades (from 1950 to 2017)[45]. Understanding climate services as “The transformation of climate-related data – together with other relevant information – into customized products such as projections, forecasts, information, trends, economic analyses, assessments (including technology assessments), counselling on best practices, development and evaluation of solutions and any other service in relation to climate that may be of use for the society at large”[46] makes this dataset a potential asset from a climate service perspective. The target beneficiaries of this dataset may include climate services providers, civil society groups, farmers, amongst different stakeholders and end-users.

Methods

Source datasets

To calculate the different climate indices, we employed two information sources: the European Climate Assessment & Dataset (ECA&D) E-OBS gridded dataset (https://www.ecad.eu/) and the ERA5 dataset (https://www.ecmwf.int/en/forecasts/datasets/reanalysis-datasets/era5). E-OBS dataset provides updated high quality daily air temperature, precipitation and sea level pressure data for Europe at different grid intervals from January 1950 onwards, with regular updates. This dataset was created from quality-controlled meteorological records[47], sourced from the European National Meteorological Services. Earlier versions of this dataset have been made available at a spatial resolution of 0.25°, being improved (0.1°) in the version v17.0e. Herein, we produced our indices at a spatial resolution of 0.25° to be consistent with the resolution of ERA5. In pursuit of the ERA4CS INDECIS project (European Union Grant 690462), daily station data from ECA&D were homogenized[48] and the adjusted records will serve as a basis for the upcoming version of E-OBS datasets. In our gridded dataset, the E-OBS dataset acted as the main base for calculating climate indices related to air temperature and precipitation. ERA5 is the fifth generation of the re-analysis dataset developed by the European Centre for Medium-Range Weather Forecasts (ECMWF)[49]. Albeit with the availability of daily air temperature and precipitation data within ERA5, our preference was made to use ERA5 as a supplementary data source to the observational datasets, with the aim of securing unavailable observational data for some climate variables. This included data for dewpoint temperature at 2 m, wind at 10 m, wind gust at 10 m, top-of-atmosphere (TOA) forcing, radiation, insolation, snow density, snow depth, snowfall, total cloud cover, and low cloud cover. Data from ERA5 were provided at a spatial resolution of 0.25° and hourly frequency. However, we aggregated the hourly data to daily scale to match the temporal resolution of E-OBS. To date, ERA5 is only available from February 1979; however, we will utilize the dataset for the early decades (1950–1978) once data is available. Figure 1 depcits the spatial coverage of the study domain;our dataset included the entire European continent, apart from Russia, Turkey and Cyprus, comprising a total of 12280 series at a spatial resolution of 0.25°.
Fig. 1

Spatial domain of the INDECISbase, the Modified Fournier Index [MFI] is represented.

Spatial domain of the INDECISbase, the Modified Fournier Index [MFI] is represented.

Index calculation

We calculated a set of 125 climate indices, based on Climlnd: a recently developed package within R platform (https://cran.r-project.org/web/packages/ClimInd/index.html). The climate indices were grouped into eight broad categories: (i) temperature-based (N = 42), (ii) precipitation-based (N = 21), (iii) bioclimatic (N = 21), (iv) wind-based (N = 5), v) aridity/continentality (N = 10), vi) snow-based (N = 12), vii) cloud/radiation-based (N = 6), and (viii) drought (N = 8). Online-only Table 1 lists these indices and their description for the eight categories. The specific formulation of each index can also be consulted via: https://cran.r-project.org/web/packages/ClimInd/ClimInd.pdf. Overall, the majority of the indices were computed on monthly, seasonal (winter: DJF, spring: MAM, summer: JJA, autumn: SON) and annual scales. However, in some instances, specific indices were calculated only on the annual scale (e.g. the growing season precipitation [GSR] and the modified Fournier index [MFI]). For those indices that require a base period for their calculation (e.g. percentile-based indices), we considered the entire period as a reference period. Herein, the 125 climate indices were computed for each one of the 12280 series covering the European continent.
Online-only Table 1

A list of the climate indices included in the INDECIS database and their main characteristics.

CategoryNameAcronymUnitsData providerStarting date
Temperature-basedMean of daily maximum air temperatureGTX°CE-OBS1950
Maximum of daily maximum air temperature TXx°CE-OBS1950
Minimum of daily maximum air temperature TXn°CE-OBS1950
Mean of daily minimum air temperatureGTN°CE-OBS1950
Maximum of daily minimum air temperature TNx°CE-OBS1950
Minimum of daily minimum air temperature TNn°CE-OBS1950
Mean of daily mean air temperatureGTG°CE-OBS1950
Maximum of daily mean air temperatureXTG°CE-OBS1950
Minimum of daily mean air temperatureNTG°CE-OBS1950
Cold days TX10p%E-OBS1950
Cold nights TN10p%E-OBS1950
Cold spell duration CSDIDaysE-OBS1950
Diurnal temperature range DTR°CE-OBS1950
Mean daily difference of diurnal temperature rangevDTR°CE-OBS1950
Frost days FDDaysE-OBS1950
Growing season length GSLDaysE-OBS1950
Ice days IDDaysE-OBS1950
Maximum consecutive frost daysCFDDaysE-OBS1950
Extreme temperature rangeETR°CE-OBS1950
Summer days SUDaysE-OBS1950
Maximum consecutive summer daysCSDDaysE-OBS1950
Difference days above/below maximum temperature 17DD17DaysE-OBS1950
Tropical nights TRDaysE-OBS1950
Heating degree daysHD17°CE-OBS1950
Very cold daysVCDDaysE-OBS1950
Very warm daysVWDDaysE-OBS1950
Warm days TX90pDaysE-OBS1950
Warm nights TN90pDaysE-OBS1950
Warm spell duration WSDIDaysE-OBS1950
Zero crossing daysZCDDaysE-OBS1950
Onset of growing season 6 daysOGS6dateE-OBS1950
Onset of growing season 10 daysOGS10dateE-OBS1950
Growing season (Apr-Oct)Ta_o°CE-OBS1950
Growing season(May-Sep)Tm_s°CE-OBS1950
Growing degree daysGD4°CE-OBS1950
Winkler indexWKI°CE-OBS1950
Winter SeverityWS°CE-OBS1950
Sum of degree days when maximum temperature > = 32STX32°CE-OBS1950
Number of days with maximum temperature > = 32D32DaysE-OBS1950
Sum of degree days when minimum temperature < = −15STN15°CE-OBS1950
Sum of degree days when minimum temperature < = −10STN10°CE-OBS1950
Sums positivePTG°CE-OBS1950
Precipitation-basedTotal precipitationRtmmE-OBS1950
Maximun precipitation RX1daymmE-OBS1950
Days precipitation ≥10 mm R10mmDaysE-OBS1950
Days precipitation ≥20 mm R20mmDaysE-OBS1950
Maximum consecutive 5-day precipitation Rx5daymmE-OBS1950
Simple daily intensity index SDIImm/DayE-OBS1950
Dry daysDDDaysE-OBS1950
Effective precipitationEPmmE-OBS1950
Longest dry period CDDDaysE-OBS1950
Longest wet period CWDDaysE-OBS1950
Precipitation fraction very wet days R95tot%E-OBS1950
Precipitation fraction extremely wet days R99tot%E-OBS1950
Heavy precipitation daysD50mmDaysE-OBS1950
Very wet daysD95pDaysE-OBS1950
Precipitation Concentration IndexPCIDimensional valuesE-OBS1950
Modified Fournier IndexMFIDimensional valuesE-OBS1950
Growing season precipitationGSRmmE-OBS1950
Non-growing season precipitationNGSRmmE-OBS1950
Total precipitation wet days PRCPTOTmmE-OBS1950
Wet days 1 mmDR1mmDaysE-OBS1950
Wet days 3 mmDR3mmDaysE-OBS1950
BioclimaticMean temperature warmest quarterBIO10°CE-OBS1950
Mean temperature coldest quarterBIO11°CE-OBS1950
Precipitation wettest monthBIO13mmE-OBS1950
Precipitation driest monthBIO14mmE-OBS1950
Coefficient of variation precipitationBIO15%E-OBS1950
Precipitation wettest quarterBIO16mmE-OBS1950
Precipitation driest quarterBIO17mmE-OBS1950
Precipitation warmest quarterBIO18mmE-OBS1950
Precipitation coldest quarterBIO19mmE-OBS1950
Temperature seasonalityBIO4°CE-OBS1950
Maximum temperature warmest monthBIO5°CE-OBS1950
Minimum temperature coldest monthBIO6°CE-OBS1950
Difference warmest/coldest monthBIO7°CE-OBS1950
Mean temperature of the wettest quarterBIO8°CE-OBS1950
Mean temperature of the driest quarterBIO9°CE-OBS1950
Mean radiationBIO20W m-2ERA51979
Universal thermal climate indexUTCI°CERA51979
Mould indexMIDaysERA51979
Heat indexHI°FE-OBS1950
Wind chill indexWCI°CERA51979
Apparent temperatureAT°CERA51979
wind-basedDays wind gusts above 21 m/sDFx21DaysERA51979
Daily maximum wind gustFXxm/sERA51979
Mean of daily mean wind strengthFGm/sERA51979
Calm daysfgcalmDaysERA51979
Days daily averaged wind above 10.8 m/sFG6BftDaysERA51979
aridity/continentality-indicesReference evapotranspirationETommERA51979
UNEP aridity indexUAIindexERA51979
Climatic moisture deficitCMDmmERA51979
De Martonne aridity indexMAIDimensional valuesE-OBS1950
Emberger aridity indexEAIDimensional valuesE-OBS1950
Johansson Continentality IndexJCIDimensional valuesE-OBS1950
Kerner Oceanity IndexKOIDimensional valuesE-OBS1950
Pinna Combinative indexPiCIDimensional valuesE-OBS1950
Budyko IndexBIDimensional valuesERA51979
Marsz Oceanity IndexMOIDimensional valuesE-OBS1950
snow-basedSnowfall sumSSmmERA51979
Snow days depth 1–10 cmSD0_10DaysERA51979
Snow days depth 10–20 cmSD10_20DaysERA51979
Frequency of snow daysFSDDayssERA51979
Mild snowy daysMSDDayssERA51979
Heavy snowy daysHSDDayssERA51979
Date of first snow coverFSCDateERA51979
Date of first permanent snow coverFPSCDateERA51979
Date of last permanent snow coverLPSCDateERA51979
Average snow depthASDmERA51979
Amount of snow covered daysSCDDaysERA51979
Maximum snow depthMSmERA51979
Cloud/radiationSum of sunshine durationSSDhERA51979
Sunny daysSNDDaysERA51979
Foggy daysFODDaysERA51979
Mean daily cloud coverCC%ERA51979
Sunshine duration fractionSSpDimensional valuesERA51979
Atmospheric Clarity IndexACI%ERA51979
DroughtStandardized precipitation index 1SPI1z unitsERA51979
Standardized precipitation index 3SPI3z unitsERA51979
Standardized precipitation index 6SPI6z unitsERA51979
Standardized precipitation index 12SPI12z unitsERA51979
Standardised Precipitation-Evapotranspiration Index 1SPEI1z unitsERA51979
Standardised Precipitation-Evapotranspiration Index 3SPEI3z unitsERA51979
Standardised Precipitation-Evapotranspiration Index 6SPEI6z unitsERA51979
Standardised Precipitation-Evapotranspiration Index 12SPEI12z unitsERA51979

The indices given in bold refer to the ETCCDI indices.

Figure 2 illustrates the spatial variability of two selected indices (Rx1day and TXx) calculated on the annual scale for three specific years. Rx1day represents the maximum precipitation gauged within one day, whilst TXx refers to the highest daily maximum air temperature recorded during the year.
Fig. 2

Spatial distribution of two selected climate indices (TXx and Rx1day) at the annual scale for three specific years (1960, 1980 and 2000).

Spatial distribution of two selected climate indices (TXx and Rx1day) at the annual scale for three specific years (1960, 1980 and 2000). Figure 3 depicts the temporal evolution of two selected climate indices (heavy precipitation days [D50mm] and the maximum consecutive frost days [CFD]) for randomly selected grid points in Europe. The two indices were computed on the annual scale for the entire study period.
Fig. 3

Temporal evolution of the annual D50mm and CFD indices calculated for specific grid points in Europe.

Temporal evolution of the annual D50mm and CFD indices calculated for specific grid points in Europe.

Data Records

The climate index dataset has been archived in figshare (10.6084/m9.figshare.c.4773491)[45], including all climate indices spanning the periods from 1950 or 1979 to 2017, based on data availability (see Online-only Table 1). Given the high number of indices included in this dataset, we have stored the climate index data in different levels. The first level corresponds to the main eight categories: temperature-based, precipitation-based, bioclimatic, wind-based, aridity/continentality, snow-based, cloud/radiation-based, and drought. Each of the first level categories (folders) is divided into subcategories (sub-folders); each of them corresponds to an individual climate index. Finally, at the third level, there are the data of each index at the different available temporal scales (i.e. monthly, seasonal and annual). The data were stored in a 3-D netcdf4 format (https://www.unidata.ucar.edu/software/netcdf/docs/netcdf_introduction.html). In specific, each file has an array of 464 (longitudes) × 201 (latitudes) × 68 (times for the annual resolution for the period 1950–2017). Indeed, the time dimension of the array varies as a function of the time resolution (i.e. monthly, seasonal, annual), as well as the period of time available (currently 1950 to 2017 for E-OBS indices and 1979 to 2017 for ERA5 indices). The geographical extent of the dataset is 25.37°N–75.37°N and 40.37°W–75.37°E. Netcdf4 files can be visualized and manipulated with several types of software, including open source software like R, Panoply, etc., and Geographic Information System software (ArcGIS©, QGIS). A complete list of the available software can be found at https://www.unidata.ucar.edu/software/netcdf/software.html. The entire dataset comprises almost 1 billion of data divided between the 125 indices and the different temporal scales (i.e. monthly, seasonal and annual).

Technical Validation

The validation of our dataset depends largely on the reliability of climatic information used for calculating each index. The quality control and homogeneity of climatic data retrieved from the source datasets (i.e. E-OBS and ERA5) are comprehensively described via https://www.ecad.eu/download/ensembles/download.php for E-OBS and https://www.ecmwf.int/en/forecasts/datasets/reanalysis-datasets/era5 for ERA5. We have checked the spatial and temporal consistency of the obtained climate indices. Also, the monthly, seasonal and annual values of the different indices were visually inspected to detect any possible problems.

Usage Notes

In addition to the stored dataset in the figshare repository, the climate indices are made also available through the project website (https://indecis.csic.es/), maintained by the Spanish National Research Council (Fig. 4). In addition to its role as a data warehouse, the project’s website can be used as a climate service, where end-user beneficiaries can select, visualize and download any index of interest for any grid point in Europe (Fig. 5). These series can be downloaded in a generic ASCII .txt format. The web site also allows for the navigation between the monthly, seasonal and annual archives and directly download any netcdf4 of the database. The entire dataset stored in this web site will be updated regularly depending on the availability and updates of the ECA&D and ERA5 data. This website is mirrored at the portal of the INDECIS project (http://www.indecis.eu/indices.php).
Fig. 4

Web-tool to visualize the INDECIS dataset and download the entire dataset corresponding to any spatial or temporal query.

Fig. 5

A representative example showing the temporal variability of a selected index (D32: annual temperature sums for days with mean temperatures above 32 °C) for a specific grid point.

Web-tool to visualize the INDECIS dataset and download the entire dataset corresponding to any spatial or temporal query. A representative example showing the temporal variability of a selected index (D32: annual temperature sums for days with mean temperatures above 32 °C) for a specific grid point.
Measurement(s)climate
Technology Type(s)computational modeling technique
Factor Type(s)air temperature • precipitation • sea level pressure • wind at 10 m • wind gust at 10 m • TOA radiation • radiation • insolation • snow density • snow depth • snowfall • total cloud cover • low cloud cover
Sample Characteristic - Environmentclimate
Sample Characteristic - LocationEurope
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