The changing climate poses a significant danger to both environment and humans. Precipitation stands out as a critical factor for impacting hydrology, ecology, agriculture, and vegetation as well as crucial for maintaining the atmospheric equilibrium. This research examined four satellite-based precipitation products spanning from 2010 to 2018, focusing on assessing the uncertainty associated with these products in Punjab Province, Pakistan. Additionally, a comparative analysis of multi-satellite-derived precipitation data was conducted for the region. Various evaluation metrics, including CC, RMSE, Bias, rBias, and POD, were employed to gauge the performance of these datasets throughout the study area. Our research yielded the following findings: (1) datasets CHIRP and SM2RAIN exhibited the capability of capturing temporal changes observed in precipitation throughout the study area. (2) All satellite-derived datasets displayed superior performance on a monthly basis compared to daily timeframes. (3) On a seasonal scale, CHIRP and SM2RAIN exhibited superior precipitation detection capabilities compared to PERSIANN-CCS and PERSIANN-CDR. (4) CHIRP and SM2RAIN exhibited superior performance across all seasons when compared to PERSIANN-CCS and PERSIANN-CDR. Nonetheless, all products exhibited reasonably accurate detection of light to moderate precipitation events. This study serves to establish a foundation for effective monitoring, mitigation, and decision-making processes.

  • Precipitation capturing performance was assessed to select the most appropriate SPPs.

  • These SPPs were not considered collectively earlier for the Punjab Province region.

  • All SPPs showed better results to capture monthly precipitation patterns instead of daily or seasonal precipitation.

  • Taylor diagrams are effective for qualitatively retrieving the spatial pattern of SPP accuracy.

Precipitation holds paramount importance as it contributes to upholding the equilibrium of the atmosphere. With the increasing frequency of hydrological disasters, there is a rising global demand for the monitoring of extreme precipitation events. Precipitation stands as a crucial element within the water cycle. Moreover, precipitation significantly impacts hydrology, environment, agricultural practices, Flora, fauna, and natural ecosystems. (Liu 2015). Hence, to gain a deeper insight into the effects of rainfall on the environment, it is essential to have access to rainfall observations with high spatial and temporal resolution. Accurate precipitation data are crucial for hydro-climatological research, the design of hydrological infrastructure, the scheduling of irrigating crops, and forecasting floods and droughts (Liu 2015).

In conventional approaches, weather radar and on-the-ground measuring stations are regarded as trustworthy sources of precipitation information (Qin et al. 2014). However, the insufficient number of ground-based stations in Punjab Province, along with their uneven distribution, presents a hurdle in obtaining consistent measurements for diverse applications (Nashwan et al. 2019). Furthermore, relying on ground-based measurements is limited by uncertainties stemming from errors introduced by factors like wind, the occurrence of missing values, and heterogeneity (Dunn et al. 2011; Guo et al. 2016; Sharifi et al. 2016). Similar limitations associated with ground-based measurements are also prevalent in the Punjab Province. Hence, it is crucial to explore reliable alternative sources of continuous precipitation data for these areas.

Over the past few years, due to the advancements in remote sensing and geo-information technology, multiple global satellite-based precipitation products (SPPs) have been developed and released for free access and they emerged as a dependable and cost-effective method for retrieving precipitation data (Nawaz et al. 2020). Consequently, it is imperative to explore alternative, trustworthy sources of continuous precipitation data from regional to global scale (Ferraro 1997; Susskind et al. 1997). SPPs can help to address the issue of sparse data in regions where ground-based measurement networks are inadequate. Additionally, they provide continuous data with high spatiotemporal resolution for global precipitation monitoring (Fang et al. 2019). These precipitation products are increasingly used in hydrology, climatology, meteorology, and other scientific studies. This is due to the fact that they have convenient data access, wide spatial coverage, accurate spatiotemporal resolutions, ongoing monitoring, and free access to both real and post-real-time data (Zhao et al. 2017). Fluctuations in rainfall patterns, combined with an increasing population, have become a significant hazard in the Punjab Province, Pakistan (Laraib et al. 2024).

Generally, algorithms utilized by SPPs retrieve precipitation data through the use of either microwave (WM) or infrared (IR) sensors (Susskind et al. 1997; Palomino-Ángel et al. 2019). Recent advancements in SPPs have yielded algorithms with the ability to provide precipitation data by integrating data from both microwave (MW) and infrared (IR) sensors (Anjum et al. 2018). These algorithms were applied in the Precipitation Estimation from Remotely Sensed Information using Artificial Neural Networks (PERSIANN) and Climate Hazards Group Infrared Precipitation (CHIRP) (Hsu et al. 1997) and these SPPs provide information about precipitation events with the highest attainable precision in both temporal (3-h intervals) and spatial (0.25°) resolutions (Moazami et al. 2013). The PERSIANN-CDR provides daily global rainfall information with a 0.25 grid resolution. The University of California's Centre for Hydrometeorology and Remote Sensing introduced this dataset in March 2000. The SM2RAIN algorithm employs a ‘bottom-up’ methodology, utilizing information from the ASCAT, SMOS, and AMSRE to calculate worldwide soil moisture levels (Cheema et al. 2011; Hou et al. 2014; Ghazanfari et al. 2016). The SM2RAIN dataset, abbreviated as SM2rain hereon, has been accessible since 2007.

SPPs provide reliable precipitation data, yet their accuracy varies based on the specific geographical region (Dembélé & Zwart 2016; Guilloteau et al. 2016). So, before putting ideas into practice, it is essential to check their accuracy. Over recent years, numerous researchers have evaluated the precision of SPPs in diverse global regions. This evaluation has been conducted in diverse locations including Africa (Guilloteau et al. 2016; Pellarin et al. 2020), Europe (Derin et al. 2016; Duan et al. 2016; Beaufort et al. 2017), America (Mourre et al. 2016; Zubieta et al. 2017; Paredes-Trejo et al. 2019) Austria (Sharifi et al. 2019), Australia (Forootan et al. 2016), China (Ullah et al. 2019; Zhang et al. 2020), Iran (Mosaffa et al. 2020), and Pakistan (Cheema & Bastiaanssen 2012; Anjum et al. 2016, 2018; Ahmed et al. 2020). Mosaffa et al. (2020) suggested utilizing PERSIANN to comprehend the spatial and temporal fluctuations of precipitation in Iran.

It's notable that the Punjab province holds significant importance in agriculture and irrigated farming in the country. Moreover, it exhibits high vulnerability to fluctuations in various meteorological parameters, with frequent occurrences of extreme weather events, making it particularly susceptible to the impacts of climate change (Khattak et al. 2015). While certain studies have evaluated the performance of PERSIANN-CDR and PERSIANN-CCS in Pakistan (Cheema et al. 2011; Anjum et al. 2016; Hussain et al. 2017), but recently developed products like SM2RAIN and CHIRP which have high spatial and temporal resolution still not considered for the Punjab Province region. The review of the literature revealed that the Punjab Province's inability to use the data from on-site meteorological stations for a variety of hydro-meteorological applications (Cheema & Bastiaanssen 2012; Anjum et al. 2018). The current study endeavors to address knowledge gaps by conducting a comprehensive multi-scale assessment of the spatiotemporal uncertainties inherent in various global precipitation products sourced from diverse origins. The primary objectives of this research are: (1) to assess the degree of uncertainty in the selected SPPs against ground-based observations within Punjab Province and (2) to examine the capturing ability of SPPs to detect the variability of extreme precipitation events. The findings of this study will be valuable for both the developers refining the algorithms of the examined satellite products and for end-users of SPPs seeking reliable data.

Study area

The Punjab Province is situated geographically at coordinates 27.70° N–34° N and 69.3° E–75.38° E, covering an area of 205,344 km2 in the northwestern region of South-central Asia in Pakistan. It constitutes 56% of the total population of the country and encompasses 26% of Pakistan's total land area. The province is subdivided into 36 districts and 9 divisions. Punjab stands as the second-largest province after Baluchistan and is bordered to the south by Sindh, to the southwest by Baluchistan, to the west by Khyber Pakhtunkhwa, and to the north by the Islamabad Capital Territory and Azad Kashmir.

In terms of topography, Punjab is primarily characterized by fertile river valleys. In the southern part, the Cholistan desert comprises barren terrain. The region boasts one of the most extensively irrigated landscapes globally, with canals crisscrossing the province. The topography of Punjab is predominantly characterized by rich alluvial plains, which have been shaped by the Indus River and its four principal tributaries in Pakistan: the Jhelum, Chenab, Ravi, and Sutlej rivers, all of which flow from north to south. Regarding climate, Punjab falls within the tropical continental region. The temperature in this region can vary from 4 to 47 °C, and the average annual precipitation measures approximately 603 mm.

Datasets

Climatological data

The daily precipitation data recorded from 26 in situ meteorological stations were obtained from the PMD for the time span spanning from 2010 to 2018. The positions of these meteorological stations can be seen in Figure 1. The PMD has verified and ensured the quality of the precipitation records. Numerous prior studies have employed the daily records from these meteorological stations for a range of hydro-climatological applications (Ahmad et al. 2018; Anjum et al. 2018; Rahman et al. 2020). Table 1 provides detailed characteristics of the in situ meteorological stations.
Table 1

List of Punjab meteorological stations

NoStationsLat (dd)Long (dd)Elevation (m)
Bahawal Nagar 30 73.24 161.05 
Bahawal Pur 29.33 71.783 110 
Bahawal Pur(A/P) 29.383 71.683 119 
Bhakkar 31.616 71.06 162 
Noorpur Thal 31.866 71.9 186 
Jauharabad 32.5 72.43 187 
Faisalabad 31.43 73.13 185.6 
Jhelum 32.93 73.73 287.19 
Khanpur 28.65 70.683 88.41 
10 Lahore A.P. 31.583 74.4 216.15 
11 Multan 30.2 71.43 121.95 
12 Mandi Bahauddin 32.96 73.8 252.97 
13 Sialkot 32.516 74.53 255.1 
14 Sialkot Airport 32.53 74.03 240 
15 Sargodha 32.05 72.66 187 
16 Toba Tek Singh 30.983 72.783 155 
17 D.G. Khan 30.05 70.63 148.1 
18 Jhang 31.26 72.316 158 
19 Mangla 33.06 73.63 283.3 
20 Sahiwal 30.65 73.16 172 
21 Chakwal 32.916 72.85 519 
22 Gujranwala 32.36 74.35 227 
23 Okara 30.8 73.43 180 
24 Rahim Yar Khan 28.43 70.316 82.93 
25 Gujrat 32.56 74.06 240 
26 Rawalpindi 33.56 73.02 508 
NoStationsLat (dd)Long (dd)Elevation (m)
Bahawal Nagar 30 73.24 161.05 
Bahawal Pur 29.33 71.783 110 
Bahawal Pur(A/P) 29.383 71.683 119 
Bhakkar 31.616 71.06 162 
Noorpur Thal 31.866 71.9 186 
Jauharabad 32.5 72.43 187 
Faisalabad 31.43 73.13 185.6 
Jhelum 32.93 73.73 287.19 
Khanpur 28.65 70.683 88.41 
10 Lahore A.P. 31.583 74.4 216.15 
11 Multan 30.2 71.43 121.95 
12 Mandi Bahauddin 32.96 73.8 252.97 
13 Sialkot 32.516 74.53 255.1 
14 Sialkot Airport 32.53 74.03 240 
15 Sargodha 32.05 72.66 187 
16 Toba Tek Singh 30.983 72.783 155 
17 D.G. Khan 30.05 70.63 148.1 
18 Jhang 31.26 72.316 158 
19 Mangla 33.06 73.63 283.3 
20 Sahiwal 30.65 73.16 172 
21 Chakwal 32.916 72.85 519 
22 Gujranwala 32.36 74.35 227 
23 Okara 30.8 73.43 180 
24 Rahim Yar Khan 28.43 70.316 82.93 
25 Gujrat 32.56 74.06 240 
26 Rawalpindi 33.56 73.02 508 
Figure 1

Location map of the Punjab Province Pakistan.

Figure 1

Location map of the Punjab Province Pakistan.

Close modal

Satellite precipitation products data

The PERSIANN dataset can give global daily precipitation data with a grid precision of 0.25°, covering a spatial range between 50° South and 50° North (Ur Rahman et al. 2018). For this study, daily precipitation evaluations from PERSIANN at a 0.25 grid scale were obtained through the CHRS website (https://chrsdata.eng.uci.edu/) for a continuous period of 8 years, spanning from 2010 to 2018. The website http://hydrology.irpi.cnr.it/download-area/sm2rain-datasets/ was utilized to acquire the daily precipitation estimates for the SM2RAIN product at a grid scale of 12.5 km. By combining the daily data, time series information for all SPPs covering monthly, seasonal, and annual periods was created. This approach aligns with previous research, in which scientists employed it to gather data at monthly, seasonal, and yearly intervals using daily precipitation estimates from SPPs.

Methods

In this research, the accuracy and uncertainty characteristics of four SPPs named as PERSIANN-CDR, PERSIANN-CCS, CHIRP, and SM2RAIN were examined in comparison to data collected at on-site meteorological stations. The study was limited to the SPP grids that had at least one relevant meteorological station for reference. Data obtained from the referenced measuring stations, spanning from January 2010 to December 2018, were employed to assess the effectiveness of SPPs across different timeframes (daily, monthly, seasonal, and annual) and spatial scales.

Statistical evaluation metrics

This study evaluated the ability of all SPPs to accurately capture the spatial variability of precipitation in Punjab Province. Various widely accepted evaluation metrics including correlation coefficients (CC), Bias, relative Bias (rBias), and root mean square error (RMSE) were employed to gauge the performance of the SPPs. These measures have been extensively employed by prior researchers to analyze the error traits of SPPs under various Weather and geographical features (Anjum et al. 2018).

CC is utilized to measure the linear association between SPPs and gauge measurements. CC values range from −1 to +1. CC value of +1 indicates a perfect positive correlation between SPPs and ground observations, while −1 signifies a perfect negative correlation. If the CC value is equal to or greater than 0.7, it signifies superior performance of SPPs with gauge measurements. The amount of precipitation was assessed using the BIAS (mm/time) to determine if it was overestimated or underestimated. Relative Bias (rBias) was used to measure the relative difference in accurately capturing precipitation events of SPPs with respect to the gauge observations usually expressed in percentage. Additionally, RMSE quantifies and evaluates the average magnitude difference (mm/time) between gauge data and satellite-derived data. A smaller RMSE value indicates that the estimated data closely align with the gauge measurements.
(1)
(2)
(3)
(4)

In the provided equations, Gi denotes the gauge-based data obtained from reference stations, while G represents the average of this gauge data. Si is for the satellite-derived estimations, S is for their average, and n stands for the overall number of observations. A satellite product is considered a perfect match for the gauge-based data when its BIAS and RMSE values are both 0, and its CC value is 1. A noteworthy analysis of SPPs has been conducted by Anjum et al. (2018). To determine the applicability of CC and rBias in hydro-climatological contexts, specific thresholds have been defined. The specified criteria for rBias and CC are ±10 and ≥0.70, respectively. Positive BIAS values indicate an underestimation of precipitation levels, while negative values indicate an overestimation. If BIAS produces negative or positive numbers, it means that the amount of precipitation has either been underestimated or overestimated.

Performance assessment approaches

A comparative analysis of probability density functions (PDFs) was conducted between satellite-derived precipitation products and reference data to assess the occurrence and statistical properties of precipitation intensity in Punjab Province. This analysis covered the period from January 2010 to December 2018, both on a daily and seasonal basis in accordance with WMO guidelines. Furthermore, Taylor diagrams, a powerful tool used to evaluate the performance of satellite products or models by comparing them to reference data, are widely used in atmospheric sciences, hydrology, climate modeling, and other geophysical disciplines to evaluate gridded data outputs. The primary purpose of using a Taylor Diagram is to visualize and evaluate the performance of multiple SPPs at a time by comparing its observations with reference data. This diagram combines three complementary statistical measures on a single plot, i.e. CC (R2), standard deviation, and RMSE with respect to the reference data. The RMSE values were depicted as angular distances from the x-axis, while the CC values were represented along the azimuthal angle.

Assessment of SPPs in monitoring the spatiotemporal variations in precipitation

Figure 2 depicts the mean daily precipitation pattern within the study region, juxtaposing information derived from meteorological stations used as references. with four satellite precipitation products (SPPs). Overall, both SPPs and gauge data show elevated levels of precipitation in the higher-altitude areas, especially in the northern to eastern section of the study area. The reference gauge data reveal elevated precipitation levels in the northeastern parts of Punjab, whereas meteorological stations situated in the western-southern areas of the study area record lower levels of precipitation. Both the PERSIANN-CCS and PERSIANN-CDR datasets tend to slightly overestimate precipitation in the west-south regions while underestimating it in the northeast. CHIRP data, based on the results, tend to slightly underestimate precipitation in both the northeastern and western-southern parts of the area. On the other hand, SM2RAIN slightly overestimates precipitation in the northern-eastern regions but underestimates it in the western-southern areas. It is worth noting that SM2RAIN performs relatively well in capturing the spatial variability of observed precipitation, particularly in low-elevation areas. However, its accuracy in reporting precipitation magnitudes in higher-altitude regions remains uncertain.
Figure 2

Comparison of the spatial variation of average daily precipitation acquired from the reference stations and four SPPs (PERSIANN-CDR, PERSIANN-CCS, SM2RAIN, and CHIRP) from 2010 to 2018.

Figure 2

Comparison of the spatial variation of average daily precipitation acquired from the reference stations and four SPPs (PERSIANN-CDR, PERSIANN-CCS, SM2RAIN, and CHIRP) from 2010 to 2018.

Close modal
Figure 3 illustrates an assessment of the temporal variations in mean daily precipitation levels derived from both reference meteorological stations and four SPPs. Moving averages were generated using daily data from the reference stations and SPPs to create a time series of rainfall data covering from 2010 to 2018. West winds and monsoon circulation systems have an impact on precipitation rates in the Punjab Province during two separate seasons, winter and summer, respectively. Two annual precipitation peaks can be seen in the reference gauge data. After analysis, it was found that the CHIRP and SM2RAIN products successfully tracked the data provided by the reference gauges, which show the existence of two-yearly peaks in precipitation. The reference data showed a range of 0.0 to 10.3 mm/day, with an average daily precipitation of 0.65 mm/day. The values of the mean daily precipitation were as follows, as determined by satellite-based data: 1.5 mm/day, ranging from 0.0 to 10.9 mm/day for CHIRP; 1.8 mm/day, ranging from 0.0 to 9.8 mm/day for PERSIANN-CDR; and 1.7 mm/day, ranging from 0.0 to 9.8 mm/day for SM2RAIN. PERSIANN-CCS tended to overestimate precipitation during the winter season and showed varying degrees of underestimation and overestimation in the summer season. On the other hand, PERSIANN-CDR frequently overestimated precipitation throughout the winter and underestimated it during the summer.
Figure 3

Comparison of the temporal variability of average daily precipitation acquired from the reference meteorological stations and four SPPs. (a) PERSIANN-CDR, (b) PERSIANN-CCS, (c) CHIRP, and (d) SM2RAIN over the Punjab from 2010 to 2018.

Figure 3

Comparison of the temporal variability of average daily precipitation acquired from the reference meteorological stations and four SPPs. (a) PERSIANN-CDR, (b) PERSIANN-CCS, (c) CHIRP, and (d) SM2RAIN over the Punjab from 2010 to 2018.

Close modal

Performance of SPPs at monthly scale

In Figure 4, the evaluation presented as a Taylor diagram concentrates on a monthly timeframe and evaluates the accuracy of four SPPs. We used normalized areal average data from both meteorological stations and SPPs to create a Taylor diagram. In comparison to PERSIANN-CCS and PERSIANN-CDR, CHIRP and SM2RAIN generally show a greater and more favorable linear correlation with the reference monthly data. The station-based data and estimations from CHIRP and SM2RAIN show CCs that are greater than 0.90, indicating a particularly high and favorable association. In contrast, the CC for PERSIANN-CCS exceeds 0.7, while for PERSIANN-CDR, it approaches 0.7, suggesting a relatively weaker correlation. Both CHIRP and SM2RAIN have RMSE values below 0.50, indicating little errors in their predictions. Conversely, the RMSE values for PERSIANN-CCS and PERSIANN-CDR exceed 0.5, signifying a higher level of error in the assessments of these products over the Punjab Province. Furthermore, the standard deviation (SD) values of CHIRP and SM2RAIN closely match the SD value of the reference data, suggesting a good agreement in terms of variability. Conversely, PERSIANN-CCS and PERSIANN-CDR exhibit some deviations from the reference data regarding variability.
Figure 4

Taylor diagram demonstrating the performances of PERSIANN-CDR, PERSIANN-CCS, SM2RAIN, and CHIRP at a monthly scale. The values of RMSE are denoted by semi-circular lines (shown in green color) and values of CC are shown by the straight blue lines.

Figure 4

Taylor diagram demonstrating the performances of PERSIANN-CDR, PERSIANN-CCS, SM2RAIN, and CHIRP at a monthly scale. The values of RMSE are denoted by semi-circular lines (shown in green color) and values of CC are shown by the straight blue lines.

Close modal
Three important metrics CC, Bias (BIAS), and RMSE are used to summarize the performance of the four SPPs at each meteorological station in Figure 5. It was established that the CC values for PERSIANN-CCS, PERSIANN-CDR, CHIRP, and SM2RAIN were, respectively, 0.55, 0.48, 0.63, and 0.79. Among these SPPs, only SM2RAIN demonstrated a good performance when compared to daily gauge-based data, while the other SPPs exhibited poorer agreements with the reference data. However, when evaluating RMSE, all SPPs showed poor performance, as indicated by their higher RMSE values, all exceeding 0.5. This suggests that none of the SPPs achieved high accuracy in estimating precipitation levels at the meteorological stations.
Figure 5

Box plots of evaluation indices (a) CC, (b) BIAS, (c) rBIAS, and (d) RMSE at a monthly scale for four satellite-based products (PERSIANN-CCS, PERSIANN-CDR, CHIRP, and SM2RAIN) over the Punjab Province range of Pakistan. Small squares denote the mean values and the horizontal lines inside the boxes indicate the median. The blue lines show the linear trend of the mean values.

Figure 5

Box plots of evaluation indices (a) CC, (b) BIAS, (c) rBIAS, and (d) RMSE at a monthly scale for four satellite-based products (PERSIANN-CCS, PERSIANN-CDR, CHIRP, and SM2RAIN) over the Punjab Province range of Pakistan. Small squares denote the mean values and the horizontal lines inside the boxes indicate the median. The blue lines show the linear trend of the mean values.

Close modal

The range of values in the CC chart was more extensive for CHIRP, signifying a wider variation, whereas for SM2RAIN, it exhibited the smallest range. This indicates that SM2RAIN demonstrated a more consistent performance in terms of correlation across the stations. In terms of BIAS, CHIRP exhibited minimal variation in its box chart, while SM2RAIN had the lowest rBIAS values compared to the other SPPs in the Punjab Province. This indicates that SM2RAIN tended to provide estimates that were closer to the observed values with less systematic bias. The CC chart displayed a broader range of values for CHIRP, indicating a wider variation. In contrast, SM2RAIN showed the smallest range, suggesting a more consistent performance in terms of correlation across the stations.

Performance of SPPs at daily scale

When compared to daily gauge precipitation data for the entire research region, Figure 6 provides an evaluation of the performance of four SPPs. For the PERSIANN-CCS, PERSIANN-CDR, CHIRP, and SM2RAIN, the CC values were determined to be 0.25, 0.30, 0.40, and 0.60, respectively. These CC values suggest poor agreements with the daily gauge data for PERSIANN-CCS and PERSIANN-CDR, indicating a weak correlation between these SPPs and the observed precipitation. All SPPs, however, display poor performance in terms of RMSE because their RMSE values are more than 0.5. This indicates that none of the SPPs achieved a high level of accuracy in estimating daily precipitation levels when in comparison to the data from gauges. This emphasizes the ongoing challenges in accurately capturing daily precipitation patterns.
Figure 6

Taylor diagram displaying the performances of the daily precipitation PERSIANN-CDR, PERSIANN-CCS, SM2RAIN, and CHIRP at a monthly scale. The values of RMSE are denoted by semi-circular lines (shown in green color) and values of CC are shown by the straight blue lines.

Figure 6

Taylor diagram displaying the performances of the daily precipitation PERSIANN-CDR, PERSIANN-CCS, SM2RAIN, and CHIRP at a monthly scale. The values of RMSE are denoted by semi-circular lines (shown in green color) and values of CC are shown by the straight blue lines.

Close modal
Figure 7 displays box plots exhibiting the CC, BIAS, and RMSE performance parameters for the four SPPs. In terms of performance in terms of correlation with daily gauge data, PERSIANN-CCS among these products has the least volatility within the spectrum of CC values. In general, all SPPs exhibit significant variability and demonstrate only a weak correlation with gauge data. PERSIANN-CCS exhibits greater variation in BIAS values when compared to other SPPs, indicating that its performance is more variable. On the contrary, CHIRP displays the least fluctuation in BIAS values, indicating a higher level of stability in its performance. However, the box length of RMSE for CHIRP reveals the greatest variability in RMSE values among the products, suggesting that CHIRP demonstrates less consistent accuracy compared to the other SPPs.
Figure 7

Box plots of evaluation indices (a) CC, (b) BIAS, (c) rBIAS, and (d) RMSE at a daily scale for four satellite-based products (PERSIANN-CCS, PERSIANN-CDR, CHIRP, and SM2RAIN) over the Punjab Province range of Pakistan. Small squares denote the mean values.

Figure 7

Box plots of evaluation indices (a) CC, (b) BIAS, (c) rBIAS, and (d) RMSE at a daily scale for four satellite-based products (PERSIANN-CCS, PERSIANN-CDR, CHIRP, and SM2RAIN) over the Punjab Province range of Pakistan. Small squares denote the mean values.

Close modal
Figure 8 depicts how elevation influences the performance of all satellite products, as assessed through metrics like CC, Bias (BIAS), relative Bias (rBIAS), and RMSE. In terms of RMSE values, it is noticeable that all SPPs show an escalation in RMSE with greater elevations. This suggests that as elevation increases, the accuracy of these SPPs in estimating precipitation tends to decrease. When it comes to CC values, as elevation increases, PERSIANN-CCS, CHIRP, and SM2RAIN show a slight increase in CC values, indicating a somewhat better correlation with observed precipitation. However, for PERSIANN-CDR, the increase in elevation leads to a more significant improvement in CC values. In terms of relative BIAS (rBIAS), as elevation rises, both PERSIANN-CCS and PERSIANN-CDR display a significant decrease in rBIAS values, indicating a reduced systematic bias at higher elevations. In contrast, CHIRP and SM2RAIN exhibit only slight decreases in rBIAS values with increasing elevation.
Figure 8

Scatter plots between the evaluation indices (CC, BIAS, rBIAS, and RMSE) on daily time scales versus elevation. Red markers represent the meteorological stations and dotted lines indicate the linear regression fitting lines.

Figure 8

Scatter plots between the evaluation indices (CC, BIAS, rBIAS, and RMSE) on daily time scales versus elevation. Red markers represent the meteorological stations and dotted lines indicate the linear regression fitting lines.

Close modal
Figure 9 portrays how the estimation metrics (CC, BIAS, rBIAS, and RMSE) of SPPs, PERSIANN-CCS, PERSIANN-CDR, CHIRP, and SM2RAIN – are influenced by the average daily precipitation, analyzed at a daily scale. In terms of RMSE, it is observed that as the precipitation rate increases, the value of RMSE also increases. This suggests that the accuracy of these SPPs tends to decrease when estimating precipitation in high-precipitation conditions. Regarding CC values, as the precipitation rate increases, both CHIRP and PERSIANN-CDR show an increase in CC values, indicating a better correlation with observed precipitation in higher precipitation scenarios. However, SM2RAIN exhibits a slight decrease in CC values as precipitation increases, implying a reduced correlation under heavy precipitation conditions. As for BIAS, the BIAS values of PERSIANN-CCS and PERSIANN-CDR decrease with increasing precipitation, suggesting a reduction in systematic bias as precipitation rates rise. Conversely, CHIRP and SM2RAIN display an increase in BIAS values with higher precipitation, indicating an increasing systematic bias under heavy precipitation conditions.
Figure 9

Scatter plots between the evaluation indices (CC, BIAS, rBIAS, and RMSE) on daily time scales versus elevation. Red markers represent the meteorological stations and dotted lines indicate the linear regression fitting lines.

Figure 9

Scatter plots between the evaluation indices (CC, BIAS, rBIAS, and RMSE) on daily time scales versus elevation. Red markers represent the meteorological stations and dotted lines indicate the linear regression fitting lines.

Close modal

Assessment of satellite products on a seasonal scale

Figure 10 depicts the seasonal changes in the computed values of CC, BIAS, and RMSE for SPPs. Significant variations in the CC box sizes imply significant variations between the reference data and the estimates given by the PERSIANN-CDR and CHIRP products throughout the spring and autumn seasons, respectively. certain fluctuations imply variances in the SPPs' association with observed precipitation, especially throughout certain seasons. According to the BIAS box dimensions for all goods, all SPPs exhibit less variance in precipitation during the autumn season as compared to the other seasons, which show significant swings in BIAS. This suggests that compared to other seasons, autumn has a more consistent agreement between the SPPs and observed data in terms of systematic bias. Additionally, the RMSE values for PERSIANN-CDR show the greatest differences among SPPs, indicating larger inaccuracies in this product's accuracy in comparison to the others across several seasons.
Figure 10

Box plots of the seasonal values of (a) CC, (b) BIAS, and (c) RMSE for four precipitation products (PERSIANN-CCS, PERSIANN-CDR, CHIRP, and SM2RAIN) over the Punjab Province range of Pakistan. Small squares denote the mean values and the horizontal lines inside the boxes indicate the median.

Figure 10

Box plots of the seasonal values of (a) CC, (b) BIAS, and (c) RMSE for four precipitation products (PERSIANN-CCS, PERSIANN-CDR, CHIRP, and SM2RAIN) over the Punjab Province range of Pakistan. Small squares denote the mean values and the horizontal lines inside the boxes indicate the median.

Close modal
Figure 11 displays the relative Biases (%) calculated for each SPP in comparison to station-based precipitation data on an annual and seasonal basis, covering the whole research region. PERSIANN-CDR and PERSIANN-CCS exhibit considerable variability in their relative biases across all seasons, with PERSIANN-CCS performing well in the summer season. On the other hand, CHIRP consistently underestimates precipitation during the winter, spring, and autumn seasons, while PERSIANN-CDR and PERSIANN-CCS tend to overestimate precipitation in these same seasons. When looking at the annual scale, both PERSIANN-CDR and SM2RAIN show acceptable levels of overestimation of precipitation. In general, the performance of CHIRP and SM2RAIN products across all seasons is relatively consistent. CHIRP slightly underestimates precipitation in the winter, spring, and autumn seasons, while SM2RAIN slightly overestimates precipitation in the winter and autumn seasons.
Figure 11

Relative Bias (rBias: %) at seasonal scale for four satellite precipitation products for the entire study area. Horizontal dashed lines are used to represent the threshold (±10%) of rBias.

Figure 11

Relative Bias (rBias: %) at seasonal scale for four satellite precipitation products for the entire study area. Horizontal dashed lines are used to represent the threshold (±10%) of rBias.

Close modal
Figure 12 shows the PDF calculated using information from both reference gauge stations and SPPs for daily precipitation events recorded in the Punjab Province. Light precipitation events (2 mm/day) were the most frequent, accounting for 86.4% of occurrences, according to a study of daily data from the reference gauges for the whole research period. Except for PERSIANN-CDR and SM2RAIN, which tend to somewhat overestimate these moderate precipitation events, all SPPs show increased performance in detecting the occurrence of events with less than 2 mm of precipitation per day. When considering seasonal fluctuations, PERSIANN-CCS and PERSIANN-CDR display greater deviations from the PDFs during the spring season. On the other hand, CHIRP and SM2RAIN exhibit the best agreement with the PDFs. Notably, spring displays the least agreement for PERSIANN-CCS and PERSIANN-CDR.
Figure 12

Probability density function (PDF) calculated for precipitation data acquired from the in situ gauges and four satellite precipitation products (PERSIANN-CCS, PERSIANN-CDR, CHIRP, and SM2RAIN) at different intensities. (a) Daily precipitation in the entire study period, (b) winter daily precipitation, (c) spring daily precipitation, (d) summer daily precipitation, and (e) autumn daily precipitation.

Figure 12

Probability density function (PDF) calculated for precipitation data acquired from the in situ gauges and four satellite precipitation products (PERSIANN-CCS, PERSIANN-CDR, CHIRP, and SM2RAIN) at different intensities. (a) Daily precipitation in the entire study period, (b) winter daily precipitation, (c) spring daily precipitation, (d) summer daily precipitation, and (e) autumn daily precipitation.

Close modal

In this study, various statistical indices and methods were chosen to thoroughly evaluate the ability of precipitation products to capture rainfall and their error characteristics across 26 stations in the Punjab Province. These indices and methods fall into three main categories: the first includes CC, which measures the agreement between satellite estimates and gauge observations; the second includes the bias, relative bias (rBias), and RMSE, which assess the error and bias of satellite estimates compared to gauge observations; and the third includes the PDF and Taylor diagram, which describe the event frequency and uncertainty of the SPPs. In situ gauge precipitation stations offer valuable data on rainfall amounts and frequency. However, their uneven spatial distribution and data inconsistencies limit their effectiveness, particularly in regions with challenging geographical environments (Kühnlein et al. 2014). To address this limitation, SPPs provide a viable alternative for precipitation estimation, offering spatially distributed data over extensive areas (Zhu et al. 2011).

Prior research has also examined the performance of these SPPs, including PERSIANN-CCS PERSIANN-CDR, and SM2RAIN in diverse climatic and topographic conditions worldwide (Moazami et al. 2013; Xu et al. 2017; Anjum et al. 2019; Rahman et al. 2019; Sharifi et al. 2019; Zhang et al. 2020). In this research, uncertainty analysis of the selected SPPs revealed that their accuracy is entirely dependent on the local topographical and environmental conditions. It is widely acknowledged that the effectiveness of SPPs is strongly influenced by local topographical and climatic conditions. Nadeem et al. (2022) also reported that the accuracy of SPPs strongly varies with in situ topography and climatic conditions. For instance, a study by Tan et al. (2015) conducted in Malaysia associated six SPPs, including PERSIANN-CDR and TRMM-3B42V7, upon investigation, it was evident that the precision of precipitation products was notably influenced by the regional climate patterns and the algorithms employed in satellite precipitation retrieval. The results of our study reinforce the idea that the performance of these satellite products is markedly influenced by the region's topography and climate conditions, which is consistent with previous research findings (Anjum et al. 2018, 2019; Ahmed et al. 2020).

Notably, our study revealed that SM2RAIN demonstrated an ability to capture spatial variations in precipitation, which stands in contrast to the findings of Asif et al. (2023) concluded that SM2RAIN effectively assessed the spatial variability of precipitation across the Pakistan range, this might be possible due to their superior morphing retrieval algorithm. Among the considered SPPs, CHIRP and SM2RAIN exhibited superior performance in characterizing the spatial variability of observed precipitation. Previously, Chiaravalloti et al. (2018) confirmed the admirable performance of PERSIANN-CDR in delineating spatial variations in precipitation when compared to other satellite products. At a daily scale, the correlations (CC) between all SPPs and the reference data were generally modest, with CC values falling below 0.61. CHIRP, SM2RAIN, PERSIANN-CCS, and PERSIANN-CDR, on the other hand, all had correlations with the reference monthly data that were greater than 0.70. This shows that, compared to daily estimations, the monthly evaluations of SPPs have more reliable agreements with the reference data. Likewise, Hamza et al. (2020) indicated that the correlations of all SPPs with the reference data on a daily scale were unsatisfactory, with values below 0.50. However, at a monthly scale, their values exceeded 0.80, suggesting improved agreements.

Regarding RMSE values, all SPPs exhibited an increase with higher elevations, signifying decreasing accuracy with increasing elevation. As the elevation increased, CC values for PERSIANN-CCS, CHIRP, and SM2RAIN slightly increased, while for PERSIANN-CDR, the increase in CC values was more significant. With increasing elevation, the relative Bias (rBIAS) of PERSIANN-CCS and PERSIANN-CDR significantly decreased compared to CHIRP and SM2RAIN, which showed slight decreases. Similarly, Xu et al. (2017) proposed that various indices (BIAS and RMSE) showed a significant correlation with topographic variations. At a monthly scale, all SPPs showed improved agreement with gauge estimations compared to the daily scale, aligning with findings from the previous study (Hamza et al. 2020). While on a seasonal scale, all SPPs demonstrated proficiency in capturing light precipitation events but during the summer season, they exhibited notable over/underestimation relative to the PDF (%). This result aligns with the previous study (Nadeem et al. 2022).

The performance and uncertainties of four commonly used SPPs were comprehensively assessed across various climatic regions by employing different statistical error metrics, including Taylor diagrams and PDF analysis, alongside ground observation-based precipitation data. This evaluation aimed to gauge the ability of these SPPs to accurately capture precipitation patterns. Our key findings can be summarized as follows:

  • After moving average analysis, it was found that the CHIRP and SM2RAIN products successfully tracked the data provided by the reference gauges with a rate of 1.5 and 1.7 mm/day, respectively.

  • On a monthly scale, CHIRP and SM2RAIN indicate a particularly high and favorable association because of their high CCs >0.90, lower RMSE value (<0.50), and closely match the SD value with reference data. While, on daily scale performance evaluation, none of these SPPs have the ability to capture accurate daily precipitation patterns when in comparison to the data from gauges.

  • It is observed that as elevation increases the accuracy of these SPPs in estimating precipitation tends were decrease. Similarly, in terms of higher precipitation scenarios, capturing accuracy of all SPPs tends to decrease in high-precipitation conditions except PERSIANN-CDR which indicates a better performance with observed precipitation.

  • On a seasonal scale, all SPPs performed better in the winter season in terms of CC (>0.5) and in the autumn season as variation in the BIAS and RMSE value is less. Based on PDF analysis, all SPPs showed better performance in detecting the occurrence of events with less than 2 mm of precipitation per day.

CHIRP and SM2RAIN emerged as the preferable solutions for hydro-meteorological investigations in the Punjab Province. In future, researchers utilize a triple collocation (TC) approach which provides reliable and continuous assessment of SPPs data over the ungauged areas. It is also suggested that the large uncertainties in satellite-based products should be paid more attention over mountainous areas where rain gauge data are insufficient.

The research work was made possible through the support of Pakistan Meteorological Department (PMD) for their valuable assistance in conducting this research.

There is no funding for this research work.

U. S. conceptualized the whole article, rendered support in data curation and formal analysis, investigated the article, developed the methodology, arranged the software, and wrote the original draft. M. L. conceptualized the whole article, rendered support in formal analysis, developed the methodology, wrote the review and edited the article. M. A. I. conceptualized the whole article, rendered support in formal analysis, developed the methodology, arranged the resources, supervised the work, wrote the review and edited the article. M. A. rendered support in data curation and formal analysis, wrote the review and edited the article. K. A. rendered support in data curation and formal analysis, supervised the article, wrote the review and edited the article. H. U. K. rendered support in formal analysis, wrote the review and edited the article. A. B. A. rendered support in formal analysis, wrote the review and edited the article. O. K. conceptualized the whole article, and wrote the review and edited the article.

This research article titled ‘ Statistical Assessment of Uncertainty and Performance of Multiple Satellite-Based Precipitation Products in Capturing Extreme Precipitation Events Across Punjab Province, Pakistan ‘ does not require an ethics statement as it pertains to a climate change study and does not involve human subjects, animal subjects, or any sensitive data that would require ethical considerations. The research is focused on performing a comparative assessment of multi-SPPs over Punjab Province, Pakistan. Therefore, no ethical approval was necessary for the conduct of this study.

Data cannot be made publicly available; readers should contact the corresponding author for details.

The authors declare there is no conflict.

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