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Udo Schneider - One of the best experts on this subject based on the ideXlab platform.
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Updated gridded datasets version 2020 provided by the Global Precipitation Climatology Centre (GPCC)
2021Co-Authors: Elke Rustemeier, Markus Ziese, Peter Finger, Udo Schneider, Andreas BeckerAbstract:<p><span>Since its founding in 1989, the Global Precipitation Climatology Centre (GPCC) has been producing global Precipitation analyses based on land surface in-situ measurements. </span><span>In the now over 30 years the underlying database has been continuously expanded and includes a high station density and large temporal coverage. Due to the semi-automatic quality control routinely performed on the incoming station data, the GPCC database has a very high quality.</span> <span>Today, the GPCC holds data from </span><span>123,000 stations, about three quarters of them having long time series.</span></p><p><span>The core of the analyses is formed by data from the global meteorological and hydrological services, which provided their records to the GPCC, as well as global and regional data collections.&#160; </span><span>In addition, the GPCC receives SYNOP and CLIMAT reports via the WMO-GTS. These form a supplement for the high quality Precipitation analyses and the basis for the near real-time evaluations.</span></p><p><span>Quality control activities include cross-referencing stations from different sources, flagging of data errors, and correcting temporally or spatially offset data. This data then forms the basis for the following interpolation and product generation.</span></p><p><span>In near real time, the 'First Guess Monthly', 'First Guess Daily', 'Monitoring Product', &#8216;Provisional Daily Precipitation Analysis&#8217; and the 'GPCC Drought Index' are generated. These are based on WMO-GTS data and monthly data generated by the CPC (NOAA). </span></p><p><span>With a 2-3 year update cycle, the high quality data products are generated with intensive quality control and built on the entire GPCC data base. These non-real time products consist of the 'Full Data Monthly', 'Full Data Daily', 'Climatology', and 'HOMPRA-Europe' and are now available in the 2020 version. </span></p><p><span>A</span><span>ll gridded datasets presented in this paper are freely available in netcdf format on the GPCC website https://gpcc.dwd.de and referenced by a digital object identifier (DOI). The site also provides an overview of all datasets, as well as a detailed description and further references for each dataset.</span></p>
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the global Precipitation Climatology project gpcp monthly analysis new version 2 3 and a review of 2017 global Precipitation
Atmosphere, 2018Co-Authors: Robert F Adler, Andreas Becker, Udo Schneider, George J Huffman, Eric J. Nelkin, Jian-jian Wang, David Bolvin, Mathew R P Sapiano, Long S Chiu, Pingping XieAbstract:The new Version 2.3 of the Global Precipitation Climatology Project (GPCP) Monthly analysis is described in terms of changes made to improve the homogeneity of the product, especially after 2002. These changes include corrections to cross-calibration of satellite data inputs and updates to the gauge analysis. Over-ocean changes starting in 2003 resulted in an overall Precipitation increase of 1.8% after 2009. Updating the gauge analysis to its final, high-quality version increases the global land total by 1.8% for the post-2002 period. These changes correct a small, incorrect dip in the estimated global Precipitation over the last decade given by the earlier Version 2.2. The GPCP analysis is also used to describe global Precipitation in 2017. The general La Nina pattern for 2017 is noted and the evolution from the early 2016 El Nino pattern is described. The 2017 global value is one of the highest for the 1979–2017 period, exceeded only by 2016 and 1998 (both El Nino years), and reinforces the small positive trend. Results for 2017 also reinforce significant trends in Precipitation intensity (on a monthly scale) in the tropics. These results for 2017 indicate the value of the GPCP analysis, in addition to research, for climate monitoring.
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evaluating the hydrological cycle over land using the newly corrected Precipitation Climatology from the global Precipitation Climatology centre gpcc
Atmosphere, 2017Co-Authors: Udo Schneider, Peter Finger, Anja Meyerchristoffer, Markus Ziese, Elke Rustemeier, Andreas BeckerAbstract:The 2015 release of the Precipitation Climatology from the Global Precipitation Climatology Centre (GPCC) for 1951–2000, based on climatological normals of about 75,100 rain gauges, allows for quantification of mean land surface Precipitation as part of the global water cycle. In GPCC’s 2011-release, a bulk climatological correction was applied to compensate for gauge undercatch. In this paper we derive an improved correction approach based on the synoptic weather reports for the period 1982–2015. The compared results show that the climatological approach tends to overestimate the correction for Central and Eastern Europe, especially in the northern winter, and in other regions throughout the year. Applying the mean weather-dependent correction to the GPCC’s uncorrected Precipitation Climatology for 1951–2000 gives a value of 854.7 mm of Precipitation per year (excluding Antarctica) or 790 mm for the global land surface. The warming of nearly 1 K relative to pre-industrial temperatures is expected to be accompanied by a 2%–3% increase in global (land and ocean) Precipitation. However, a comparison of Climatology for 30-year reference periods from 1931–1960 up to 1981–2010 reveals no significant trend for land surface Precipitation. This may be caused by the large variability of Precipitation, the varying data coverage over time and other issues related to the sampling of rain-gauge networks. The GPCC continues to enlarge and further improve the quality of its database, and will generate Precipitation analyses with homogeneous data coverage over time. Another way to reduce the sampling issues is the combination of rain gauge-based analyses with remote sensing (i.e., satellite or radar) datasets.
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The new portfolio of global Precipitation data products of the Global Precipitation Climatology Centre suitable to assess and quantify the global water cycle and resources
Proceedings of the International Association of Hydrological Sciences, 2016Co-Authors: Udo Schneider, Peter Finger, Markus Ziese, Elke Rustemeier, Anja Meyer-christoffer, Andreas BeckerAbstract:Abstract. Precipitation plays an important role in the global energy and water cycle. Accurate knowledge of Precipitation amounts reaching the land surface is of special importance for fresh water assessment and management related to land use, agriculture and hydrology, incl. risk reduction of flood and drought. High interest in long-term Precipitation analyses arises from the needs to assess climate change and its impacts on all spatial scales. In this framework, the Global Precipitation Climatology Centre (GPCC) has been established in 1989 on request of the World Meteorological Organization (WMO). It is operated by Deutscher Wetterdienst (DWD, National Meteorological Service of Germany) as a German contribution to the World Climate Research Programme (WCRP). This paper provides information on the most recent update of GPCC's gridded data product portfolio including example use cases.
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gpcc s new land surface Precipitation Climatology based on quality controlled in situ data and its role in quantifying the global water cycle
Theoretical and Applied Climatology, 2014Co-Authors: Udo Schneider, Andreas Becker, Peter Finger, Anja Meyerchristoffer, Markus Ziese, B Rudolf, Udo Schneider, B RudolfAbstract:In 1989, the need for reliable gridded land surface Precipitation data sets, in view of the large uncertainties in the assessment of the global energy and water cycle, has led to the establishment of the Global Precipitation Climatology Centre (GPCC) at Deutscher Wetterdienst on invitation of the WMO. The GPCC has calculated a Precipitation Climatology for the global land areas for the target period 1951–2000 by objective analysis of climatological normals of about 67,200 rain gauge stations from its data base. GPCC's new Precipitation Climatology is compared to several other station-based Precipitation climatologies as well as to Precipitation climatologies derived from the GPCP V2.2 data set and from ECMWF's model reanalyses ERA-40 and ERA-Interim. Finally, how GPCC's best estimate for terrestrial mean Precipitation derived from the Precipitation Climatology of 786 mm per year (equivalent to a water transport of 117,000 km3) is fitting into the global water cycle context is discussed.
B Rudolf - One of the best experts on this subject based on the ideXlab platform.
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gpcc s new land surface Precipitation Climatology based on quality controlled in situ data and its role in quantifying the global water cycle
Theoretical and Applied Climatology, 2014Co-Authors: Udo Schneider, Andreas Becker, Peter Finger, Anja Meyerchristoffer, Markus Ziese, B Rudolf, Udo Schneider, B RudolfAbstract:In 1989, the need for reliable gridded land surface Precipitation data sets, in view of the large uncertainties in the assessment of the global energy and water cycle, has led to the establishment of the Global Precipitation Climatology Centre (GPCC) at Deutscher Wetterdienst on invitation of the WMO. The GPCC has calculated a Precipitation Climatology for the global land areas for the target period 1951–2000 by objective analysis of climatological normals of about 67,200 rain gauge stations from its data base. GPCC's new Precipitation Climatology is compared to several other station-based Precipitation climatologies as well as to Precipitation climatologies derived from the GPCP V2.2 data set and from ECMWF's model reanalyses ERA-40 and ERA-Interim. Finally, how GPCC's best estimate for terrestrial mean Precipitation derived from the Precipitation Climatology of 786 mm per year (equivalent to a water transport of 117,000 km3) is fitting into the global water cycle context is discussed.
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a description of the global land surface Precipitation data products of the global Precipitation Climatology centre with sample applications including centennial trend analysis from 1901 present
Earth System Science Data, 2013Co-Authors: Andreas Becker, Peter Finger, Anja Meyerchristoffer, B Rudolf, Kirstin Schamm, Udo Schneider, Markus ZieseAbstract:Abstract. The availability of highly accessible and reliable monthly gridded data sets of global land-surface Precipitation is a need that was already identified in the mid-1980s when there was a complete lack of globally homogeneous gauge-based Precipitation analyses. Since 1989, the Global Precipitation Climatology Centre (GPCC) has built up its unique capacity to assemble, quality assure, and analyse rain gauge data gathered from all over the world. The resulting database has exceeded 200 yr in temporal coverage and has acquired data from more than 85 000 stations worldwide. Based on this database, this paper provides the reference publication for the four globally gridded monthly Precipitation products of the GPCC, covering a 111-yr analysis period from 1901–present. As required for a reference publication, the content of the product portfolio, as well as the underlying methodologies to process and interpolate are detailed. Moreover, we provide information on the systematic and statistical errors associated with the data products. Finally, sample applications provide potential users of GPCC data products with suitable advice on capabilities and constraints of the gridded data sets. In doing so, the capabilities to access El Nino–Southern Oscillation (ENSO) and North Atlantic Oscillation (NAO) sensitive Precipitation regions and to perform trend analyses across the past 110 yr are demonstrated. The four gridded products, i.e. the Climatology (CLIM) V2011, the Full Data Reanalysis (FD) V6, the Monitoring Product (MP) V4, and the First Guess Product (FG), are publicly available on easily accessible latitude/longitude grids encoded in zipped clear text ASCII files for subsequent visualization and download through the GPCC download gate hosted on ftp://ftp.dwd.de/pub/data/gpcc/html/download_gate.html by the Deutscher Wetterdienst (DWD), Offenbach, Germany. Depending on the product, four (0.25°, 0.5°, 1.0°, 2.5° for CLIM), three (0.5°, 1.0°, 2.5°, for FD), two (1.0°, 2.5° for MP) or one (1.0° for FG) resolution is provided, and for each product a DOI reference is provided allowing for public user access to the products. A preliminary description of the scope of a fifth product – the Homogenized Precipitation Analysis (HOMPRA) – is also provided. Its comprehensive description will be submitted later in an extra paper upon completion of this data product. DOIs of the gridded data sets examined are as follows: doi:10.5676/DWD_GPCC/CLIM_M_V2011_025 , doi:10.5676/DWD_GPCC/CLIM_M_V2011_050 , doi:10.5676/DWD_GPCC/CLIM_M_V2011_100 , doi:10.5676/DWD_GPCC/CLIM_M_V2011_250 , doi:10.5676/DWD_GPCC/FD_M_V6_050 , doi:10.5676/DWD_GPCC/FD_M_V6_100 , doi:10.5676/DWD_GPCC/FD_M_V6_250 , doi:10.5676/DWD_GPCC/MP_M_V4_100 , doi:10.5676/DWD_GPCC/MP_M_V4_250 , doi:10.5676/DWD_GPCC/FG_M_100 .
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The Global Precipitation Climatology Centre (GPCC) - in situ observation based Precipitation Climatology on regional and global scale
2009Co-Authors: T. Fuchs, U. Schneider, B RudolfAbstract:The Global Precipitation Climatology Centre (GPCC, http://gpcc.dwd.de) provides global monthly Precipitation analyses for monitoring and research of the earth’s climate. The centre is a German contribution to the World Climate Research Programme (WCRP), to the Global Climate Observing System (GCOS), and to the Global Earth Observation System of Systems (GEOSS). It contributes to water resources assessments, flood and drought monitoring, climate variability and trend analyses. GPCC published in year 2008 a new global Precipitation Climatology as well as a reanalysis of its full data base for all months of the period 1901-2007.
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the version 2 global Precipitation Climatology project gpcp monthly Precipitation analysis 1979 present
Journal of Hydrometeorology, 2003Co-Authors: Robert F Adler, B Rudolf, Udo Schneider, John E Janowiak, George J Huffman, A T C Chang, Ralph Ferraro, Pingping Xie, Scott Curtis, David BolvinAbstract:Abstract The Global Precipitation Climatology Project (GPCP) Version-2 Monthly Precipitation Analysis is described. This globally complete, monthly analysis of surface Precipitation at 2.5° latitude × 2.5° longitude resolution is available from January 1979 to the present. It is a merged analysis that incorporates Precipitation estimates from low-orbit satellite microwave data, geosynchronous-orbit satellite infrared data, and surface rain gauge observations. The merging approach utilizes the higher accuracy of the low-orbit microwave observations to calibrate, or adjust, the more frequent geosynchronous infrared observations. The dataset is extended back into the premicrowave era (before mid-1987) by using infrared-only observations calibrated to the microwave-based analysis of the later years. The combined satellite-based product is adjusted by the rain gauge analysis. The dataset archive also contains the individual input fields, a combined satellite estimate, and error estimates for each field. This m...
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The New 20-Year Global Precipitation Climatology Project (GPCP) Merged Satellite and Rainguage Monthly Analysis
1999Co-Authors: Robert F Adler, B Rudolf, George J Huffman, Arnold Gruber, Pingping Xie, John E JanowiakAbstract:A new 20-year, monthly, globally complete Precipitation analysis has been completed as part of the World Climate Research Program's (WCRP/GEWEX) Global Precipitation Climatology Project (GPCP). This Version 2 of the community generated data set is a result of combining the procedures and data sets as described. The global, monthly, 2.5x 2.5 degree latitude-longitude product utilizes Precipitation estimates from low-orbit microwave sensors (SSM/1) and geosynchronous IR sensors and raingauge information over land. The low-orbit microwave estimates are used to adjust or correct the geosynchronous IR estimates, thereby maximizing the utility of the more physically-based microwave estimates and the finer time sampling of the geosynchronous observations. Information from raingauges is blended into the analyses over land. In the 1986-present period TOVS-based Precipitation estimates are adjusted to GPCP fields and used in polar regions to produce globally-complete results. The extension back to 1979 utilizes the procedures of Xie and Arkin and their OLR Precipitation Index (OPI). The 20-year Climatology of the Version 2 GPCP analysis indicates the expected features of a very strong Pacific Ocean ITCZ and SPCZ with maximum 20-year means approaching 10 mm/day. A similar strength maximum over land is evident over Borneo. Weaker maxima in the tropics occur in the Atlantic ITCZ and over South America and Africa. In mid-latitudes of the Northern Hemisphere the Western Pacific and Western Atlantic maxima have values of approximately 7 mm/day, while in the Southern Hemisphere the mid-latitude maxima are located southeast of Africa, in mid-Pacific as an extension of the SPCZ and southeast of South America. In terms of global totals the GPCP analysis shows 2.7 mm/day (3.0 mm/day over ocean; 2.1 mm/day over land), similar to the Jaeger Climatology, but not other climatologies. Zonal averages peak at 6 mm/day at 7*N with mid-latitude peaks of about 3 mm/day at 40-45* latitude. Poleward of 45* the GPCP analysis shows larger zonally-averaged values than most previous satellite-based estimates, although the values are similar to tl,ie Jaeger Climatology. Over both ocean areas and at high latitudes the analysis requires additional validation and comparison with special, independent data sets from field experiments and from the Tropical Rain Measuring Mission (TRMM) to confirm the absolute magnitude and variations of Precipitation seen in the analysis. Interannual and other variations of the global fields will be shown focusing on the recent ('97-'99) ENSO event compared with previous events, including teleconnections at mid and high latitudes. An ENSO Precipitation Index (ESPI) calculated using the new data set will be described and related to the evolution of the ENSO events during the 20-year period.
Robert F Adler - One of the best experts on this subject based on the ideXlab platform.
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The Global Precipitation Climatology Project Version 3 Products
2021Co-Authors: George J Huffman, Robert F Adler, Ali Behrangi, David Bolvin, Eric J. Nelkin, Yang Song, Jian-jian WangAbstract:<p>The Global Precipitation Climatology Project (GPCP) is currently providing a next-generation Version 3.1 Monthly product, which covers the period 1983-2019.&#160; This modernized product includes higher spatial resolution (0.5&#176;x0.5&#176;); a wider coverage (60&#176;N-S) by geosynchronous IR estimates, now based on the Precipitation Estimation from Remotely Sensed Information using Artificial Neural Networks-Climate Data Record (PERSIANN-CDR) algorithm, with monthly recalibration using Goddard Profiling (GPROF) algorithm retrievals from selected passive microwave sensors; and improved calibrations of Television-Infrared Operational Satellite (TIROS) Operational Vertical Sounder (TOVS) and Advanced Infrared Sounder (AIRS) Precipitation, used outside 60&#186;N-S.&#160; The merged satellite estimate is adjusted to the Tropical Combined Climatology (TCC) at lower latitudes, and the Merged CloudSat, TRMM, and GPM (MCTG) Climatology at higher latitudes.&#160; Finally, V3.1 provides a merger of the satellite-only estimates with the Global Precipitation Climatology Centre (GPCC) monthly 1&#176;x1&#176; gauge analyses.&#160;</p><p>As well, the GPCP team is advancing a companion global Version 3 Daily product, in which the Integrated Multi-satellitE Retrievals for Global Precipitation Measurement (GPM) mission (IMERG) Final Run V06 estimates are used where available (initially restricted to 60&#176;N-S), and rescaled TOVS/AIRS data in high-latitude areas, all calibrated to the GPCP V3.1 Monthly estimate.&#160; Since IMERG currently extends back to June 2000, daily PERSIANN-CDR data will be used for the period January 1983&#8211;May 2000 to complete the record.</p><p>This presentation will provide early results for, and the latest status of, the Monthly and Daily GPCP products as a function of time and region.&#160; Key points include examining homogeneity over time and across time and space boundaries between input datasets.&#160; One key activity is to refine the V3 products while we continue to produce the Version 2 GPCP products for on-going use.</p>
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the global Precipitation Climatology project gpcp monthly analysis new version 2 3 and a review of 2017 global Precipitation
Atmosphere, 2018Co-Authors: Robert F Adler, Andreas Becker, Udo Schneider, George J Huffman, Eric J. Nelkin, Jian-jian Wang, David Bolvin, Mathew R P Sapiano, Long S Chiu, Pingping XieAbstract:The new Version 2.3 of the Global Precipitation Climatology Project (GPCP) Monthly analysis is described in terms of changes made to improve the homogeneity of the product, especially after 2002. These changes include corrections to cross-calibration of satellite data inputs and updates to the gauge analysis. Over-ocean changes starting in 2003 resulted in an overall Precipitation increase of 1.8% after 2009. Updating the gauge analysis to its final, high-quality version increases the global land total by 1.8% for the post-2002 period. These changes correct a small, incorrect dip in the estimated global Precipitation over the last decade given by the earlier Version 2.2. The GPCP analysis is also used to describe global Precipitation in 2017. The general La Nina pattern for 2017 is noted and the evolution from the early 2016 El Nino pattern is described. The 2017 global value is one of the highest for the 1979–2017 period, exceeded only by 2016 and 1998 (both El Nino years), and reinforces the small positive trend. Results for 2017 also reinforce significant trends in Precipitation intensity (on a monthly scale) in the tropics. These results for 2017 indicate the value of the GPCP analysis, in addition to research, for climate monitoring.
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Estimating Climatological Bias Errors for the Global Precipitation Climatology Project (GPCP)
Journal of Applied Meteorology and Climatology, 2012Co-Authors: Robert F Adler, George J HuffmanAbstract:AbstractA procedure is described to estimate bias errors for mean Precipitation by using multiple estimates from different algorithms, satellite sources, and merged products. The Global Precipitation Climatology Project (GPCP) monthly product is used as a base Precipitation estimate, with other input products included when they are within ±50% of the GPCP estimates on a zonal-mean basis (ocean and land separately). The standard deviation σ of the included products is then taken to be the estimated systematic, or bias, error. The results allow one to examine monthly climatologies and the annual Climatology, producing maps of estimated bias errors, zonal-mean errors, and estimated errors over large areas such as ocean and land for both the tropics and the globe. For ocean areas, where there is the largest question as to absolute magnitude of Precipitation, the analysis shows spatial variations in the estimated bias errors, indicating areas where one should have more or less confidence in the mean precipitat...
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The Global Precipitation Climatology Project (GPCP): Results, Status and Future
2007Co-Authors: Robert F AdlerAbstract:The Global Precipitation Climatology Project (GPCP) is one of a number of long-term, satellite-based, global analyses routinely produced under the auspices of the World Climate Research Program (WCRP) and its Global Energy and Watercycle EXperiment (GEWEX) program. The research quality analyses are produced a few months after real-time through the efforts of scientists at various national agencies and universities in the U.S., Europe and Japan. The primary product is a monthly analysis of surface Precipitation that is globally complete and spans the period 1979-present. There are also pentad analyses for the same period and a daily analysis for the 1997-present period. Although generated with somewhat different data sets and analysis schemes, the pentad and daily data sets are forced to agree with the primary monthly analysis on a grid box by grid box basis. The primary input data sets are from low-orbit passive microwave observations, geostationary infrared observations and surface raingauge information. Examples of research with the data sets are discussed, focusing on tropical (25N-25s) rainfall variations and possible long-term changes in the 28-year (1979-2006) monthly dataset. Techniques are used to discriminate among the variations due to ENSO, volcanic events and possible long-term changes for rainfall over both land and ocean. The impact of the two major volcanic eruptions over the past 25 years is estimated to be about a 5% maximum reduction in tropical rainfall during each event. Although the global change of Precipitation in the data set is near zero, a small upward linear change over tropical ocean (0.06 mm/day/l0yr) and a slight downward linear change over tropical land (-0.03 mm/day/l0yr) are examined to understand the impact of the inhomogeneity in the data record and the length of the data set. These positive changes correspond to about a 5% increase (ocean) and 3% increase (ocean plus land) during this time period. Relations between variations in surface temperature and Precipitation are analyzed on seasonal to inter-decadal time scales. A new, version 3 of GPCP is being planned to incorporate new satellite information (e.g., TRMM) and provide higher spatial and temporal resolution for at least part of the data record. The goals and plans for that GPCP re-processing will be outlined.
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the version 2 global Precipitation Climatology project gpcp monthly Precipitation analysis 1979 present
Journal of Hydrometeorology, 2003Co-Authors: Robert F Adler, B Rudolf, Udo Schneider, John E Janowiak, George J Huffman, A T C Chang, Ralph Ferraro, Pingping Xie, Scott Curtis, David BolvinAbstract:Abstract The Global Precipitation Climatology Project (GPCP) Version-2 Monthly Precipitation Analysis is described. This globally complete, monthly analysis of surface Precipitation at 2.5° latitude × 2.5° longitude resolution is available from January 1979 to the present. It is a merged analysis that incorporates Precipitation estimates from low-orbit satellite microwave data, geosynchronous-orbit satellite infrared data, and surface rain gauge observations. The merging approach utilizes the higher accuracy of the low-orbit microwave observations to calibrate, or adjust, the more frequent geosynchronous infrared observations. The dataset is extended back into the premicrowave era (before mid-1987) by using infrared-only observations calibrated to the microwave-based analysis of the later years. The combined satellite-based product is adjusted by the rain gauge analysis. The dataset archive also contains the individual input fields, a combined satellite estimate, and error estimates for each field. This m...
George J Huffman - One of the best experts on this subject based on the ideXlab platform.
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The Global Precipitation Climatology Project Version 3 Products
2021Co-Authors: George J Huffman, Robert F Adler, Ali Behrangi, David Bolvin, Eric J. Nelkin, Yang Song, Jian-jian WangAbstract:<p>The Global Precipitation Climatology Project (GPCP) is currently providing a next-generation Version 3.1 Monthly product, which covers the period 1983-2019.&#160; This modernized product includes higher spatial resolution (0.5&#176;x0.5&#176;); a wider coverage (60&#176;N-S) by geosynchronous IR estimates, now based on the Precipitation Estimation from Remotely Sensed Information using Artificial Neural Networks-Climate Data Record (PERSIANN-CDR) algorithm, with monthly recalibration using Goddard Profiling (GPROF) algorithm retrievals from selected passive microwave sensors; and improved calibrations of Television-Infrared Operational Satellite (TIROS) Operational Vertical Sounder (TOVS) and Advanced Infrared Sounder (AIRS) Precipitation, used outside 60&#186;N-S.&#160; The merged satellite estimate is adjusted to the Tropical Combined Climatology (TCC) at lower latitudes, and the Merged CloudSat, TRMM, and GPM (MCTG) Climatology at higher latitudes.&#160; Finally, V3.1 provides a merger of the satellite-only estimates with the Global Precipitation Climatology Centre (GPCC) monthly 1&#176;x1&#176; gauge analyses.&#160;</p><p>As well, the GPCP team is advancing a companion global Version 3 Daily product, in which the Integrated Multi-satellitE Retrievals for Global Precipitation Measurement (GPM) mission (IMERG) Final Run V06 estimates are used where available (initially restricted to 60&#176;N-S), and rescaled TOVS/AIRS data in high-latitude areas, all calibrated to the GPCP V3.1 Monthly estimate.&#160; Since IMERG currently extends back to June 2000, daily PERSIANN-CDR data will be used for the period January 1983&#8211;May 2000 to complete the record.</p><p>This presentation will provide early results for, and the latest status of, the Monthly and Daily GPCP products as a function of time and region.&#160; Key points include examining homogeneity over time and across time and space boundaries between input datasets.&#160; One key activity is to refine the V3 products while we continue to produce the Version 2 GPCP products for on-going use.</p>
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the global Precipitation Climatology project gpcp monthly analysis new version 2 3 and a review of 2017 global Precipitation
Atmosphere, 2018Co-Authors: Robert F Adler, Andreas Becker, Udo Schneider, George J Huffman, Eric J. Nelkin, Jian-jian Wang, David Bolvin, Mathew R P Sapiano, Long S Chiu, Pingping XieAbstract:The new Version 2.3 of the Global Precipitation Climatology Project (GPCP) Monthly analysis is described in terms of changes made to improve the homogeneity of the product, especially after 2002. These changes include corrections to cross-calibration of satellite data inputs and updates to the gauge analysis. Over-ocean changes starting in 2003 resulted in an overall Precipitation increase of 1.8% after 2009. Updating the gauge analysis to its final, high-quality version increases the global land total by 1.8% for the post-2002 period. These changes correct a small, incorrect dip in the estimated global Precipitation over the last decade given by the earlier Version 2.2. The GPCP analysis is also used to describe global Precipitation in 2017. The general La Nina pattern for 2017 is noted and the evolution from the early 2016 El Nino pattern is described. The 2017 global value is one of the highest for the 1979–2017 period, exceeded only by 2016 and 1998 (both El Nino years), and reinforces the small positive trend. Results for 2017 also reinforce significant trends in Precipitation intensity (on a monthly scale) in the tropics. These results for 2017 indicate the value of the GPCP analysis, in addition to research, for climate monitoring.
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Estimating Climatological Bias Errors for the Global Precipitation Climatology Project (GPCP)
Journal of Applied Meteorology and Climatology, 2012Co-Authors: Robert F Adler, George J HuffmanAbstract:AbstractA procedure is described to estimate bias errors for mean Precipitation by using multiple estimates from different algorithms, satellite sources, and merged products. The Global Precipitation Climatology Project (GPCP) monthly product is used as a base Precipitation estimate, with other input products included when they are within ±50% of the GPCP estimates on a zonal-mean basis (ocean and land separately). The standard deviation σ of the included products is then taken to be the estimated systematic, or bias, error. The results allow one to examine monthly climatologies and the annual Climatology, producing maps of estimated bias errors, zonal-mean errors, and estimated errors over large areas such as ocean and land for both the tropics and the globe. For ocean areas, where there is the largest question as to absolute magnitude of Precipitation, the analysis shows spatial variations in the estimated bias errors, indicating areas where one should have more or less confidence in the mean precipitat...
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the version 2 global Precipitation Climatology project gpcp monthly Precipitation analysis 1979 present
Journal of Hydrometeorology, 2003Co-Authors: Robert F Adler, B Rudolf, Udo Schneider, John E Janowiak, George J Huffman, A T C Chang, Ralph Ferraro, Pingping Xie, Scott Curtis, David BolvinAbstract:Abstract The Global Precipitation Climatology Project (GPCP) Version-2 Monthly Precipitation Analysis is described. This globally complete, monthly analysis of surface Precipitation at 2.5° latitude × 2.5° longitude resolution is available from January 1979 to the present. It is a merged analysis that incorporates Precipitation estimates from low-orbit satellite microwave data, geosynchronous-orbit satellite infrared data, and surface rain gauge observations. The merging approach utilizes the higher accuracy of the low-orbit microwave observations to calibrate, or adjust, the more frequent geosynchronous infrared observations. The dataset is extended back into the premicrowave era (before mid-1987) by using infrared-only observations calibrated to the microwave-based analysis of the later years. The combined satellite-based product is adjusted by the rain gauge analysis. The dataset archive also contains the individual input fields, a combined satellite estimate, and error estimates for each field. This m...
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Global Monthly and Daily Precipitation Analysis for the Global Precipitation Climatology Project (GPCP): Global and Regional Variations and Trends
2001Co-Authors: Robert F Adler, George J Huffman, Eric J. Nelkin, Scott Curtis, David Bolvin, Franco EinaudiAbstract:The 22 year, monthly, globally complete Precipitation analysis of the World Climate Research Program's (WCRP/GEWEX) Global Precipitation Climatology Project (GPCP) and the four year (1997-present) daily GPCP analysis are described in terms of the data sets and analysis techniques used in their preparation. These analyses are then used to study global and regional variations and trends during the 22 years and the shorter-time scale events that constitute those variations. The GPCP monthly data set shows no significant trend in global Precipitation over the twenty years, unlike the positive trend in global surface temperatures over the past century. The global trend analysis must be interpreted carefully, however, because the inhomogeneity of the data set makes detecting a small signal very difficult, especially over this relatively short period. The relation of global (and tropical) total Precipitation and ENSO (El Nino and Southern Oscillation) events is quantified with no significant signal when land and ocean are combined. In terms of regional trends 1979 to 2000 the tropics have a distribution of regional rainfall trends that has an ENSO-like pattern with features of both the El Nino and La Nina. This feature is related to a possible trend in the frequency of ENSO events (either El Nino or La Nina) over the past 20 years. Monthly anomalies of Precipitation are related to ENSO variations with clear signals extending into middle and high latitudes of both hemispheres. The El Nino and La Nina mean anomalies are near mirror images of each other and when combined produce an ENSO signal with significant spatial continuity over large distances. A number of the features are shown to extend into high latitudes. Positive anomalies extend in the Southern Hemisphere from the Pacific southeastward across Chile and Argentina into the south Atlantic Ocean. In the Northern Hemisphere the counterpart feature extends across the southern U.S. and Atlantic Ocean into Europe. In the Southern Hemisphere an anomaly feature is shown to spiral into the Antarctica land mass. The extremes of ENSO-related anomalies are also examined and indicate that globally, during both El Nino and La Nina, more extremes of Precipitation (both wet and dry) occur than during the "neutral" regime, with the El Nino regime showing larger magnitudes. The distribution is different for the globe as a whole and when the area is restricted to just land. The recent (1998-present) Tropical Rainfall Measuring Mission (TRMM) observations are also compared with the GPCP analyses and are evaluated with regard to improving the long-term GPCP data set.
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spatial and temporal variability of Precipitation over the mediterranean basin based on 32 year satellite global Precipitation Climatology project data part i evaluation and climatological patterns
International Journal of Climatology, 2016Co-Authors: Nikolaos Hatzianastassiou, John D. Pnevmatikos, C. D. Papadimas, Christos J. Lolis, Aristides Bartzokas, Vincenzo Levizzani, B. D. KatsoulisAbstract:The Precipitation regime over the Mediterranean basin is investigated for the period 1979–2010 using monthly mean satellite data from the Global Precipitation Climatology Project (GPCPv2). The results show that a clear contrast exists between the more rainy northern part of the study region (Southern Europe) and the drier southern area (North Africa, Iberian Peninsula) and between the western sides (rainsides) of the Iberian, Italian and Balkan peninsulas and their eastern sides (rainshadows). The mean annual Precipitation averaged over the study area is P = 593 ± 203 mm year−1, but it has a strong spatial variability ranging from 20 mm year−1 (North Africa) to 1500 mm year−1 (Alps). A significant seasonal variability exists, with the early winter and late autumn months (November and December) being the wettest with Precipitation amounts larger than 60 mm month−1. The GPCPv2 satellite Precipitation data are satisfactorily correlated with rain gauge measurements from 433 stations within the study area (correlation coefficient R = 0.78 for all stations on a yearly basis, with values ranging between 0.72 and 0.82, depending on the season) with a slight overestimation. They also compare well with the higher spatial and temporal resolution Tropical Rainfall Measuring Mission (TRMM) data, which supports the validity of the present study.
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Spatial and temporal variability of Precipitation over the Mediterranean Basin based on 32-year satellite Global Precipitation Climatology Project data. Part-II: inter-annual variability and trends
International Journal of Climatology, 2016Co-Authors: Nikolaos Hatzianastassiou, John D. Pnevmatikos, C. D. Papadimas, Christos J. Lolis, Aristides Bartzokas, Vincenzo Levizzani, B. D. KatsoulisAbstract:Monthly mean satellite data from the Global Precipitation Climatology Project (GPCPv2) are used to examine the year-by-year variability of Precipitation over the Mediterranean Basin and its changes over the period 1979–2010. The results show that the mean annual Precipitation averaged over the study area has slightly increased from 1979 to 2010 by 1.28 mm or by 0.2% (trend not statistically significant at the 95% confidence level). Nevertheless, examining the trends at a local scale, spatial and temporal patterns are revealed, with opposite trends in adjacent areas and increasing Precipitation in summer and autumn against almost unchanged or decreasing Precipitation in winter and spring, respectively. Inter-decadal changes of Precipitation are detected, with Precipitation decreasing in the 1980s, then increasing through the late 1990s and finally declining in the 2000s before levelling off since 2007. These changes are significantly anti-correlated (R = −0.57, up to −0.66 in winter) with the North Atlantic Oscillation (NAO) index, thus confirming the critical role of this large-scale teleconnection for the regional Precipitation over the basin.
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Spatial and temporal variability of Precipitation over the Mediterranean Basin based on 32‐year satellite Global Precipitation Climatology Project data, part I: evaluation and climatological patterns
International Journal of Climatology, 2016Co-Authors: Nikolaos Hatzianastassiou, John D. Pnevmatikos, C. D. Papadimas, Christos J. Lolis, Aristides Bartzokas, Vincenzo Levizzani, B. D. KatsoulisAbstract:The Precipitation regime over the Mediterranean basin is investigated for the period 1979–2010 using monthly mean satellite data from the Global Precipitation Climatology Project (GPCPv2). The results show that a clear contrast exists between the more rainy northern part of the study region (Southern Europe) and the drier southern area (North Africa, Iberian Peninsula) and between the western sides (rainsides) of the Iberian, Italian and Balkan peninsulas and their eastern sides (rainshadows). The mean annual Precipitation averaged over the study area is P = 593 ± 203 mm year−1, but it has a strong spatial variability ranging from 20 mm year−1 (North Africa) to 1500 mm year−1 (Alps). A significant seasonal variability exists, with the early winter and late autumn months (November and December) being the wettest with Precipitation amounts larger than 60 mm month−1. The GPCPv2 satellite Precipitation data are satisfactorily correlated with rain gauge measurements from 433 stations within the study area (correlation coefficient R = 0.78 for all stations on a yearly basis, with values ranging between 0.72 and 0.82, depending on the season) with a slight overestimation. They also compare well with the higher spatial and temporal resolution Tropical Rainfall Measuring Mission (TRMM) data, which supports the validity of the present study.
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Spatial and Temporal Variation of Precipitation in Greece and Surrounding Regions Based on Global Precipitation Climatology Project Data
Journal of Climate, 2008Co-Authors: Nikolaos Hatzianastassiou, B. D. Katsoulis, John D. Pnevmatikos, V. AntakisAbstract:Abstract In this study, the spatial and temporal distribution of Precipitation in the broader Greek area is investigated for the 26-yr period 1979–2004 by using monthly mean satellite-based data, with complete spatial coverage, taken from the Global Precipitation Climatology Project (GPCP). The results show that there exists a clear contrast between the more rainy western Greek area (rainside) and the drier eastern one (rainshadow), whereas there is little Precipitation over the islands, particularly in the southern parts. The computed long-term areal mean annual Precipitation amount averaged for the study area is equal to P = 639.8 ± 44.8 mm yr−1, showing a decreasing trend of −2.32 mm yr−1 or −60.3 mm over the 26-yr study period, which corresponds to −9.4%. This decrease of Precipitation, arising primarily in winter and secondarily in spring, is the result of a decreasing trend from 1979 through the 1980s, against an increase during the 1990s through the early 2000s, followed again by a decrease up to t...