dc.description.abstract |
Being a developing country, Afghanistan faces many challenges in managing its water
resources. The analysis and management of water resources have been greatly hampered by
the absence of high-resolution precipitation data. Using observational data from 68 stations
over a 24-year period (1961-1984), this study attempts to produce a long-term (60 years) high
spatial resolution 0.08 ° monthly bias-corrected gridded precipitation dataset for Afghanistan.
In addition to taking the relationships between adjacent stations into account, gridded and
reanalysis products containing data records for the relevant period were chosen for the monthly
statistical comparison with the observed data. Through the application of concerned linear
regression equations, the datasets that produced the best relationships were employed to close
the gap in the base period (1961–1984). With a grid resolution of 0.08 degrees, the gape-filled
data was interpolated on the GIS interface using the ordinary kriging (OK) spatial interpolation
tool. Following the creation of the observed reference dataset, the GPCC, Aphrodite, ERA5-
Land, and University of Delaware gridded datasets were subjected to commonly used statistical
measures for the evaluation of their correctness on a grid-to-grid basis for the selection of the
best dataset for bias-correction of the onwards data. Before applying monthly bias-correction
factors to the remaining data, linear scaling and quantile mapping approaches were statistically
assessed. Additionally, the study intends to assess the accuracy of two recently observed data
from the Afghanistan Meteorological Department (AMD) and Agromet utilizing records from
21 and 16 stations during periods of 14 and 10 years, respectively. Using the Mann-Kendel test
and Sen's slope methodology, the created long-term observed precipitation record was used to
identify the annual and seasonal spatial trend. The findings revealed that the GPCC
outperformed alternative datasets across the entirety of Afghanistan, with the exception of a
few regions in the central west, mainly Bamiyan and Daikundi, as well as eastern Badakhshan
and, southern Paktika. The average biased R2 and KGE between the observed and GPCC
increased from 0.80 and 0.51 to 0.85 and 0.88, respectively, thanks to linear scaling, which was
also able to reduce the mean absolute error from 9.25 to 6.35. The dataset developed was
further used for the Annual and seasonal trend analysis over Afghanistan. In eastern, southern,
and central parts of Afghanistan, 40.40 % of the area produced a significant increase in annual
precipitation ranging from (0.78 - 16) mm/year, while decreases from (-0.31 -11.85) mm/year
were observed in Baghlan, Bamian, Sari pul, Ghor Zabul, Badghis, Southern Paktika, and
eastern Badakhshan. Along the Pakistani border, where the monsoon rains fall, and in elevatedvii
places, where the most precipitation falls, a growing tendency was noted. Mostly Afghanistan's
eastern, central, and southern regions have significant increasing trends during the summer
(JJA) and autumn (SON), ranging from 0.15 to 5.2 mm/year, while other parts of the nation
experience little to no decreasing trends in these seasons. The winter months in Kunar saw the
greatest seasonal rise in precipitation, up to 5.25 mm/year, with the summer months in eastern
Paktika seeing an increase of 5.15 mm/year. Engineers and scientists may use the dataset
created, evaluation of gridded datasets, and trend analysis as a tool to predict future climatic
scenarios, address water management concerns, and analyse water availability, supply, and
demand using various hydro climatological tools. |
en_US |
dc.subject |
Key words: Gridded dataset, Kriging, DJF, MAM, JJA, SON, Precipitation, Afghanistan, Trend Analysis |
en_US |