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Evaluating the Effectiveness of Phase Difference in Early Drought Detection


Article Information

Title: Evaluating the Effectiveness of Phase Difference in Early Drought Detection

Authors: Nawai Habib, Abu Talha Manzoor, Sawaid Abbas, Syed Muhammad Irteza

Journal: International Journal of Innovations in Science & Technology

HEC Recognition History
Category From To
Y 2024-10-01 2025-12-31
Y 2023-07-01 2024-09-30
Y 2021-07-01 2022-06-30

Publisher: 50SEA JOURNALS (SMC-PRIVATE) LIMITED

Country: Pakistan

Year: 2024

Volume: 6

Issue: 6

Language: English

Keywords: DroughtRainfallNDVILag TimeThar dessert

Categories

Abstract

Introduction. This research work focuses on how various phase relationships can enhance our understanding of the effects of drought on moisture deficiency in desert ecosystems, an extensive and damaging environmental phenomenon that affects natural ecosystems, economies, health, agriculture, and society.
Novelty Statement. The primary objective of this research is to inspect the lag time variance between fixed and dynamic lag windows correlated with NDVI, aiming to devise an optimal methodology for drought analysis in this region.  
Material and Methods. Leveraging remote sensing data, this study delves into the complex drought dynamics of the Thar Desert, employing a comprehensive analysis of 22 years of CHIRPS rainfall time series data and MODIS NDVI (Normalized Difference Vegetation Index) product. This study performed a cross-correlation of rainfall and NDVI, comparing the lag time difference between fixed lag windows (16, 32, 48, 64 days) and dynamic lag windows (ranging from 4 to 64 days with incremental steps) against 22 years of NDVI data of MODIS.
Results and Discussions. The preliminary results showed that dynamic lag windows of 4, 8, 12, 16, …, and 64 days exhibit the highest correlation with NDVI, with a lag time of 40 days showing maximum correlation. These findings suggest that dynamic lag windows capture the temporal variability of drought impact on vegetation more effectively compared to fixed lag windows in the Thar Desert. The same work was done with a sub-dynamic lag window ranging in between the highly correlated lag episodes of dynamic and fix windows respectively i.e.,40 days and 48 days, concluding that a lag phase of 42 days exhibits the highest correlation with vegetation more effectively. Furthermore, the study unveils a significant drought event in 2002, showcasing the sensitivity of the dynamic lag approach in detecting extreme drought occurrences.
Concluding Remarks. This research not only advances drought analysis methodologies in arid regions but also underscores the imperative for future investigations to explore the generalizability of dynamic lag windows across diverse regions and evaluate their predictive capacity in forecasting drought-induced vegetation changes.


Research Objective

To evaluate the variance in lag times between fixed and dynamic lag windows correlated with NDVI, aiming to develop an optimal methodology for drought analysis in the Thar Desert.


Methodology

The study utilized 22 years of CHIRPS rainfall time series data and MODIS NDVI product for the Thar Desert. Rainfall data was aggregated to a biweekly (16-day) interval and resampled to 250 meters. NDVI data was also processed at a 16-day interval and 250m resolution. Savitzky-Golay filtering was applied to NDVI data to remove anomalies. Lagged precipitation was computed for fixed (16, 32, 48, 64 days), dynamic (4 to 64 days), and sub-dynamic (36 to 44 days) windows. Pearson Cross-Correlation (PCC) analysis was used to assess the relationship between precipitation and NDVI time series at different lag times.

Methodology Flowchart
                        graph TD
    A[Data Acquisition: CHIRPS Rainfall & MODIS NDVI] --> B[Data Preprocessing: Aggregation, Resampling, Filtering]
    B --> C[Lag Window Analysis: Fixed, Dynamic, Sub-Dynamic]
    C --> D[Pearson Cross-Correlation PCC Calculation]
    D --> E[Identify Optimal Lag Time]
    E --> F[Analyze Drought Events & Vegetation Response]
    F --> G[Draw Conclusions & Recommendations]                    

Discussion

The study emphasizes that the timing of rainfall (lag time) is crucial for understanding drought impacts on vegetation. Dynamic lag windows provide a more accurate view of the association between plant health and rainfall compared to fixed windows. The optimal lag time in the Thar Desert was found to be approximately 40 days, with a peak at 42 days when considering the most effective fixed and dynamic windows. This precision is vital for effective drought monitoring and improving drought coping strategies.


Key Findings

Dynamic lag windows (4, 8, 12, 16, and 64 days) showed the highest correlation with NDVI, with a lag time of 40 days exhibiting maximum correlation. A sub-dynamic lag window, incorporating the highly correlated lag episodes of 40 and 48 days, revealed that a lag phase of 42 days provided the highest correlation with vegetation. A significant drought event in 2002 was identified, highlighting the sensitivity of the dynamic lag approach.


Conclusion

Dynamic lag windows are more effective than fixed lag windows for analyzing drought impacts on vegetation in the Thar Desert. A 42-day lag phase in a sub-dynamic window shows the highest correlation with vegetation dynamics. Future research should explore the applicability of dynamic lag windows in diverse regions and assess their predictive capacity for drought-induced vegetation changes. Expanding drought indicators to include temperature, evapotranspiration, and soil moisture could provide a more comprehensive understanding of drought dynamics.


Fact Check

* The study analyzed 22 years of CHIRPS rainfall and MODIS NDVI data. (Confirmed by text: "analyzing 22 years of CHIRPS rainfall time series data and MODIS NDVI product" and "over a 22-year period from 2001 to 2022").
* The Thar Desert experiences minimal precipitation averaging between 100 and 500 millimeters annually. (Confirmed by text: "minimal precipitation averaging between 100 and 500 millimeters annually").
* A significant drought period was observed in 2002 and 2003. (Confirmed by text: "a significant drought period with below-average annual precipitation rates was observed in 2002 and 2003").


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