Figure 4 | Scientific Reports

Figure 4

From: Contribution of changing precipitation and climatic oscillations in explaining variability of water extents of large reservoirs in Pakistan

Figure 4

ERA and APH data based linear trends for Mangla-Jhelum basin, Tarbela-Indus basin and overall basin. The ERA based Tp and APH based Ap show a significant decrease of 5.38 mm year−1, 4.68 mm year−1, 8.40 mm year−1 and 319 km2 year−1, 310 km2 year−1 and 358 km2 year−1, respectively. Two very strong El Niño events of 1982–1983 and 1997–1998 reduced Tp (from 481 mm year−1 to 292 mm year−1 and 591 mm year−1 to 446 mm year−1 for 1982–1983 and 1997–1998). A similar decrease in Tp has been observed for Mangla-Jhelum basin during 1982–1983 and 1997–1998 (from 358 mm year−1 to 292 mm year−1 and 438 mm year−1 to 346 mm year−1, respectively). The Ap also decreased from 50233 km2 year−1 to 42442 km2 year−1 and 48286 km2 year−1 to 39758 km2 year−1 for Tarbela during 1982–1983, and 1997–1998. Mangla also shows a decrease in Ap during 1982–1983, 1997–1998 and 2007 (44180 km2 year−1 to 38432 km2 year−1, 40199 km2 year−1 to 34740 km2 year−1 and 36543 km2 year−1 to 30230 km2 year−1, respectively). Strength of ENSO phases are represented by VS (very strong), S (strong), M (moderate), W (weak) and N (neutral).

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