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Figures/A. Ardalan and Hashemifaraz - 2024 - Uncovering sea level patterns in Caspian Sea altimetry data/figure_01.txt

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+The number of SSH observations in 675 time series from 1 Hz GDR data of TOPEX/Poseidon, Jason1, Jason2, and Jason3 missions over the Caspian Sea. The time series are spaced at 6 km intervals. Garabogaz Gulf is not included because it has a different sea level variation mechanism.

Figures/A. Ardalan and Hashemifaraz - 2024 - Uncovering sea level patterns in Caspian Sea altimetry data/figure_02.txt

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+Time series of SSH data before and after outlier removal by the Baarda method. The first column shows the original SSH data. The second column shows the SSH data with outliers removed and the trend polynomial of degree 8 fitted.

Figures/A. Ardalan and Hashemifaraz - 2024 - Uncovering sea level patterns in Caspian Sea altimetry data/figure_03.txt

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+The epochs of trend changing points for four time periods around 1995, 2000, 2005, and 2020 at the time series locations along the altimetry tracks.

Figures/A. Ardalan and Hashemifaraz - 2024 - Uncovering sea level patterns in Caspian Sea altimetry data/figure_04.txt

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+The main-track and the main-cross-overs used for filtering the trend changing epochs.

Figures/A. Ardalan and Hashemifaraz - 2024 - Uncovering sea level patterns in Caspian Sea altimetry data/figure_05.txt

@@ -0,0 +1 @@
+The trend changing epochs for four periods at the main-track and main-cross-overs and their neighboring time series within 30 km radius.

Figures/A. Ardalan and Hashemifaraz - 2024 - Uncovering sea level patterns in Caspian Sea altimetry data/figure_06.txt

@@ -0,0 +1 @@
+The four trend changing epochs of Caspian Sea level fluctuations after the filtering procedure. The name of rivers are also shown as indicators of drainage areas. The tracks that are not shown are those that were filtered out due to inconsistent trend changing epochs.

Figures/A. Ardalan and Hashemifaraz - 2024 - Uncovering sea level patterns in Caspian Sea altimetry data/figure_07.txt

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+Flowchart of classification of water drainage areas.

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+        },
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+        },
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+        },
+        {
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+        },
+        {
+          "text": "(1)",
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+        }
+      ]
+    },
+    {
+      "text": "The SSH observations in this study include the following corrections: atmospheric (dry and wet), ionospheric, tide (solid",
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+        {
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+        },
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+        },
+        {
+          "text": "ionospheric,",
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+        },
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+        },
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+          "text": "(solid",
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+        }
+      ]
+    },
+    {
+      "text": "and pole), sea surface topography fluctuations, and sea state bias. We exclude the ocean tide and load corrections, because",
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+        545.46,
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+      "words": [
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+          "text": "and",
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+            58.59,
+            265.59
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+        },
+        {
+          "text": "pole),",
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+            265.59
+          ]
+        },
+        {
+          "text": "sea",
+          "bbox_points": [
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+            265.59
+          ]
+        },
+        {
+          "text": "surface",
+          "bbox_points": [
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+            256.57,
+            131.91,
+            265.59
+          ]
+        },
+        {
+          "text": "topography",
+          "bbox_points": [
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+            256.57,
+            180.79,
+            265.59
+          ]
+        },
+        {
+          "text": "fluctuations,",
+          "bbox_points": [
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+            256.25,
+            233.35,
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+          ]
+        },
+        {
+          "text": "and",
+          "bbox_points": [
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+            251.41,
+            265.59
+          ]
+        },
+        {
+          "text": "sea",
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+            267.25,
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+          ]
+        },
+        {
+          "text": "state",
+          "bbox_points": [
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+          ]
+        },
+        {
+          "text": "bias.",
+          "bbox_points": [
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+            309.89,
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+          ]
+        },
+        {
+          "text": "We",
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+            265.59
+          ]
+        },
+        {
+          "text": "exclude",
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+            360.49,
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+          ]
+        },
+        {
+          "text": "the",
+          "bbox_points": [
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+            376.14,
+            265.59
+          ]
+        },
+        {
+          "text": "ocean",
+          "bbox_points": [
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+            403.22,
+            265.59
+          ]
+        },
+        {
+          "text": "tide",
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+        },
+        {
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+        },
+        {
+          "text": "load",
+          "bbox_points": [
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+        },
+        {
+          "text": "corrections,",
+          "bbox_points": [
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+            265.59
+          ]
+        },
+        {
+          "text": "because",
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+            256.57,
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+          ]
+        }
+      ]
+    },
+    {
+      "text": "the Caspian Sea is a closed basin with no tidal variations, and it is too far from the oceans to experience any tidal load effect.",
+      "bbox_points": [
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+      "words": [
+        {
+          "text": "the",
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+            269.61,
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+          ]
+        },
+        {
+          "text": "Caspian",
+          "bbox_points": [
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+        },
+        {
+          "text": "Sea",
+          "bbox_points": [
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+            269.61,
+            108.23,
+            278.62
+          ]
+        },
+        {
+          "text": "is",
+          "bbox_points": [
+            110.67,
+            269.61,
+            117.03,
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+          ]
+        },
+        {
+          "text": "a",
+          "bbox_points": [
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+            269.61,
+            124.13,
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+          ]
+        },
+        {
+          "text": "closed",
+          "bbox_points": [
+            126.48,
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+          ]
+        },
+        {
+          "text": "basin",
+          "bbox_points": [
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+          ]
+        },
+        {
+          "text": "with",
+          "bbox_points": [
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+          ]
+        },
+        {
+          "text": "no",
+          "bbox_points": [
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+        },
+        {
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+        },
+        {
+          "text": "variations,",
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+            269.61,
+            274.23,
+            278.62
+          ]
+        },
+        {
+          "text": "and",
+          "bbox_points": [
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+            269.61,
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+        },
+        {
+          "text": "it",
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+        },
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+        },
+        {
+          "text": "too",
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+            324.11,
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+          ]
+        },
+        {
+          "text": "far",
+          "bbox_points": [
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+            269.61,
+            337.6,
+            278.62
+          ]
+        },
+        {
+          "text": "from",
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+            269.61,
+            359.31,
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+        },
+        {
+          "text": "the",
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+        },
+        {
+          "text": "oceans",
+          "bbox_points": [
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+            404.81,
+            278.62
+          ]
+        },
+        {
+          "text": "to",
+          "bbox_points": [
+            407.18,
+            269.61,
+            415.22,
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+          ]
+        },
+        {
+          "text": "experience",
+          "bbox_points": [
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+            269.61,
+            461.37,
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+          ]
+        },
+        {
+          "text": "any",
+          "bbox_points": [
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+          ]
+        },
+        {
+          "text": "tidal",
+          "bbox_points": [
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+            498.73,
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+          ]
+        },
+        {
+          "text": "load",
+          "bbox_points": [
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+            518.77,
+            278.62
+          ]
+        },
+        {
+          "text": "effect.",
+          "bbox_points": [
+            521.19,
+            269.61,
+            545.45,
+            278.62
+          ]
+        }
+      ]
+    },
+    {
+      "text": "We also exclude the inverse barometer correction, because the non-tidal water bodies have periodic signals mainly caused by",
+      "bbox_points": [
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+        282.59,
+        545.46,
+        291.61
+      ],
+      "words": [
+        {
+          "text": "We",
+          "bbox_points": [
+            43.43,
+            282.59,
+            57.3,
+            291.61
+          ]
+        },
+        {
+          "text": "also",
+          "bbox_points": [
+            59.59,
+            282.59,
+            75.78,
+            291.61
+          ]
+        },
+        {
+          "text": "exclude",
+          "bbox_points": [
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+            282.59,
+            109.11,
+            291.61
+          ]
+        },
+        {
+          "text": "the",
+          "bbox_points": [
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+            282.59,
+            124.2,
+            291.61
+          ]
+        },
+        {
+          "text": "inverse",
+          "bbox_points": [
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+          ]
+        },
+        {
+          "text": "barometer",
+          "bbox_points": [
+            157.78,
+            282.59,
+            199.35,
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+          ]
+        },
+        {
+          "text": "correction,",
+          "bbox_points": [
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+            291.61
+          ]
+        },
+        {
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+            291.61
+          ]
+        },
+        {
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+        },
+        {
+          "text": "non-tidal",
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+        },
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+        },
+        {
+          "text": "bodies",
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+            386.99,
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+          ]
+        },
+        {
+          "text": "have",
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+            408.39,
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+        },
+        {
+          "text": "periodic",
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+        },
+        {
+          "text": "signals",
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+          ]
+        },
+        {
+          "text": "mainly",
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+        },
+        {
+          "text": "caused",
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+        {
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+        }
+      ]
+    },
+    {
+      "text": "atmospheric and hydrodynamic effects, and these signals do not influence trend modeling. By excluding the inverse barom-",
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+        295.26,
+        545.45,
+        304.59
+      ],
+      "words": [
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+        },
+        {
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+        },
+        {
+          "text": "hydrodynamic",
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+            172.44,
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+        },
+        {
+          "text": "effects,",
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+          ]
+        },
+        {
+          "text": "and",
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+          ]
+        },
+        {
+          "text": "these",
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+          ]
+        },
+        {
+          "text": "signals",
+          "bbox_points": [
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+        },
+        {
+          "text": "do",
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+        },
+        {
+          "text": "not",
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+          ]
+        },
+        {
+          "text": "influence",
+          "bbox_points": [
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+          ]
+        },
+        {
+          "text": "trend",
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+          ]
+        },
+        {
+          "text": "modeling.",
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+          ]
+        },
+        {
+          "text": "By",
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+          ]
+        },
+        {
+          "text": "excluding",
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+        },
+        {
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+        },
+        {
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+            304.59
+          ]
+        },
+        {
+          "text": "barom-",
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+            295.57,
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+            304.59
+          ]
+        }
+      ]
+    },
+    {
+      "text": "eter correction, we also avoid possible errors in the SSH observations due to the correction’s imperfection. We will",
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+        },
+        {
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+        {
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+        },
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+        },
+        {
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+          ]
+        },
+        {
+          "text": "possible",
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+        },
+        {
+          "text": "errors",
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+        },
+        {
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+        },
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+        {
+          "text": "correction’s",
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+        },
+        {
+          "text": "imperfection.",
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+    },
+    {
+      "text": "demonstrate that our mathematical model can successfully separate the trend, which is our signal of interest, from the per-",
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+        {
+          "text": "can",
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+        },
+        {
+          "text": "successfully",
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+        },
+        {
+          "text": "separate",
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+        },
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+        },
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+          "text": "trend,",
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+        },
+        {
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+        },
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+        },
+        {
+          "text": "signal",
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+        },
+        {
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+        },
+        {
+          "text": "interest,",
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+        },
+        {
+          "text": "from",
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+        },
+        {
+          "text": "the",
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+        },
+        {
+          "text": "per-",
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+        }
+      ]
+    },
+    {
+      "text": "iodic effects.",
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+      "words": [
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+          "text": "iodic",
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+        },
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+          "text": "effects.",
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+        }
+      ]
+    },
+    {
+      "text": "3. TIME SERIES DEVELOPMENT",
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+      "words": [
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+        {
+          "text": "TIME",
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+        },
+        {
+          "text": "SERIES",
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+        },
+        {
+          "text": "DEVELOPMENT",
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+        }
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+    {
+      "text": "We followed these steps to build the time series from the repeated SSH observations within all cycles of the selected satellite",
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+        }
+      ]
+    },
+    {
+      "text": "altimetry missions. First, we selected the tracks that cover our research area. Then, we used the coordinates of 1 Hz obser-",
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+          "text": "First,",
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+    },
+    {
+      "text": "vations along the tracks from one cycle as the reference points for our time series development. We identified and",
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+}

Figures/A. Ardalan and Hashemifaraz - 2024 - Uncovering sea level patterns in Caspian Sea altimetry data/table_01.txt

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+Satellite altimetry missions, the data versions, durations, and cycles that are used for this study

Figures/A. Ardalan and Hashemifaraz - 2024 - Uncovering sea level patterns in Caspian Sea altimetry data/table_02.json

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Figures/A. Ardalan and Hashemifaraz - 2024 - Uncovering sea level patterns in Caspian Sea altimetry data/table_02.txt

@@ -0,0 +1 @@
+Summary statistics of the number of observations in 675 time series from 1 Hz GDR data of TOPEX/Poseidon, Jason1, Jason2, and

Figures/Abadi et al. - 2024 - Hydrogeochemical characterization of groundwater in mountainous catchment and its suitability for dr/figure_01.txt

@@ -0,0 +1 @@
+Location map of the study area: The map includes surface drainage map, water sampling points, settlement and elevation map.

Figures/Abadi et al. - 2024 - Hydrogeochemical characterization of groundwater in mountainous catchment and its suitability for dr/figure_02.txt

@@ -0,0 +1 @@
+Geological and structural map of the study area. The structure exhibits different lineament folds and faults.

Figures/Abadi et al. - 2024 - Hydrogeochemical characterization of groundwater in mountainous catchment and its suitability for dr/figure_03.txt

@@ -0,0 +1 @@
+Spatial distribution map of chemical parameters: (a) pH, (b) total alkalinity, (c) total hardness and (d) total dissolved solids of groundwater samples in March 2020.

Figures/Abadi et al. - 2024 - Hydrogeochemical characterization of groundwater in mountainous catchment and its suitability for dr/figure_04.txt

@@ -0,0 +1 @@
+Spatial distribution map of chemical parameters: (a) calcium, (b) magnesium, (c) sodium and (d) potassium of groundwater samples in March 2020.

Figures/Abadi et al. - 2024 - Hydrogeochemical characterization of groundwater in mountainous catchment and its suitability for dr/figure_05.txt

@@ -0,0 +1 @@
+Spatial distribution map of chemical parameters: (a) sulfate, (b) bicarbonate, (c) chloride and (d) fluoride of groundwater samples in March 2020.

Figures/Abadi et al. - 2024 - Hydrogeochemical characterization of groundwater in mountainous catchment and its suitability for dr/figure_06.txt

@@ -0,0 +1 @@
+Spatial distribution map of chemical parameters: (a) nitrate and (b) nitrite of groundwater samples in March 2020.

Figures/Abadi et al. - 2024 - Hydrogeochemical characterization of groundwater in mountainous catchment and its suitability for dr/figure_07.txt

@@ -0,0 +1 @@
+(a) Piper diagram and (b) Schoeller diagrams of groundwater samples from Irob region in March 2020.

Figures/Abadi et al. - 2024 - Hydrogeochemical characterization of groundwater in mountainous catchment and its suitability for dr/figure_08.txt

@@ -0,0 +1 @@
+Gibbs diagrams indicating the water chemistry natural evolution mechanisms and showing the water–rock inter- action is the dominant process: (a) TDS versus Naþ þ Kþ/(Naþþ Ca2þ þ Kþ) and (b) TDS versus Cl/(Clþ HCO

Figures/Abadi et al. - 2024 - Hydrogeochemical characterization of groundwater in mountainous catchment and its suitability for dr/figure_09.txt

@@ -0,0 +1 @@
+Scatter diagrams groundwater samples from the study area for hydro geochemical evolution processes: (a) scatter plot between Ca2þ þ Mg2þ and HCO

Figures/Abadi et al. - 2024 - Hydrogeochemical characterization of groundwater in mountainous catchment and its suitability for dr/figure_10.txt

@@ -0,0 +1 @@
+Scatter diagrams of groundwater samples from the study area for hydro geochemical evolution processes: (a) scatter plot between Naþ and Cl, (b) scatter plot between Ca2þ and Mg2þ, (c) scatter plot between Cl and NO

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+            152.85,
+            243.43,
+            160.86
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+        },
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+            152.85,
+            460.39,
+            160.86
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+        }
+      ]
+    },
+    {
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+        449.56,
+        174.87
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+            166.85,
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+        },
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+        },
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+            166.85,
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+      ]
+    },
+    {
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+        449.56,
+        188.87
+      ],
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+        },
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+        },
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+            180.85,
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+            188.87
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+        },
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+            237.02,
+            188.87
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+        },
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+            180.85,
+            291.68,
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+        },
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+        },
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+            180.85,
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+        }
+      ]
+    },
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+        449.56,
+        202.87
+      ],
+      "words": [
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+        },
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+          "bbox_points": [
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+            194.86,
+            188.83,
+            202.87
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+        },
+        {
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+            202.87
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+        },
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+        }
+      ]
+    },
+    {
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+        207.14,
+        445.15,
+        216.88
+      ],
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+        },
+        {
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+            216.88
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+            208.86,
+            188.83,
+            216.88
+          ]
+        },
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+            216.88
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+        {
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+            208.86,
+            291.68,
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+        },
+        {
+          "text": "150",
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+            208.86,
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+            216.88
+          ]
+        },
+        {
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+            208.86,
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+            216.88
+          ]
+        }
+      ]
+    },
+    {
+      "text": "Naþ 19.1 51 34.3 9.98 200 0",
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+        221.15,
+        445.15,
+        230.88
+      ],
+      "words": [
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+        },
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+            222.86,
+            184.41,
+            230.88
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+            222.86,
+            287.26,
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+        },
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+            222.86,
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+        }
+      ]
+    },
+    {
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+      "bbox_points": [
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+        235.15,
+        455.98,
+        244.88
+      ],
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+            195.24,
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+        },
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+        },
+        {
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+        },
+        {
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+            236.87,
+            333.51,
+            244.88
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+        },
+        {
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+    {
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+        250.87,
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+    },
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+            254.92,
+            93.4,
+            260.53
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+      ]
+    },
+    {
+      "text": "165 433.1 307 87.38 300 60",
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+        449.56,
+        258.89
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+            250.87,
+            144.95,
+            258.89
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+            250.87,
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+        },
+        {
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+    },
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+        268.92,
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+            268.92,
+            85.41,
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+        264.82,
+        460.39,
+        272.83
+      ],
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+            264.82,
+            296.09,
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+        {
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+        },
+        {
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+        },
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+      "bbox_points": [
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+        292.82,
+        84.35,
+        300.84
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+            292.82,
+            84.35,
+            300.84
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+      ]
+    },
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+        87.39,
+        302.54
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+            296.93,
+            87.39,
+            302.54
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+        }
+      ]
+    },
+    {
+      "text": "15.2 37.21 20.5 5.92 50 0",
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+        445.15,
+        300.84
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+      "words": [
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+          "bbox_points": [
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+            146.95,
+            300.84
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+        },
+        {
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+        },
+        {
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+        },
+        {
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+            300.84
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+        },
+        {
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+        },
+        {
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+            292.82,
+            445.15,
+            300.84
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+        }
+      ]
+    },
+    {
+      "text": "NO",
+      "bbox_points": [
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+        306.83,
+        84.35,
+        314.84
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+      "words": [
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+            84.35,
+            314.84
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+        }
+      ]
+    },
+    {
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+        87.39,
+        316.54
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+            310.93,
+            87.39,
+            316.54
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+        }
+      ]
+    },
+    {
+      "text": "0.02 0.18 0.07 0.05 3 0",
+      "bbox_points": [
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+        306.83,
+        445.15,
+        314.84
+      ],
+      "words": [
+        {
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+          "bbox_points": [
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+            306.83,
+            146.95,
+            314.84
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+        },
+        {
+          "text": "0.18",
+          "bbox_points": [
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+            306.83,
+            190.83,
+            314.84
+          ]
+        },
+        {
+          "text": "0.07",
+          "bbox_points": [
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+            306.83,
+            239.01,
+            314.84
+          ]
+        },
+        {
+          "text": "0.05",
+          "bbox_points": [
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+            306.83,
+            287.26,
+            314.84
+          ]
+        },
+        {
+          "text": "3",
+          "bbox_points": [
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+            306.83,
+            329.1,
+            314.84
+          ]
+        },
+        {
+          "text": "0",
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+            306.83,
+            445.15,
+            314.84
+          ]
+        }
+      ]
+    },
+    {
+      "text": "F 0.16 1.31 0.52 0.33 1.5 0",
+      "bbox_points": [
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+        320.83,
+        445.15,
+        328.84
+      ],
+      "words": [
+        {
+          "text": "F",
+          "bbox_points": [
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+            75.61,
+            328.84
+          ]
+        },
+        {
+          "text": "0.16",
+          "bbox_points": [
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+            320.83,
+            146.95,
+            328.84
+          ]
+        },
+        {
+          "text": "1.31",
+          "bbox_points": [
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+            320.83,
+            190.83,
+            328.84
+          ]
+        },
+        {
+          "text": "0.52",
+          "bbox_points": [
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+            320.83,
+            239.01,
+            328.84
+          ]
+        },
+        {
+          "text": "0.33",
+          "bbox_points": [
+            272.01,
+            320.83,
+            287.26,
+            328.84
+          ]
+        },
+        {
+          "text": "1.5",
+          "bbox_points": [
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+            320.83,
+            335.51,
+            328.84
+          ]
+        },
+        {
+          "text": "0",
+          "bbox_points": [
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+            320.83,
+            445.15,
+            328.84
+          ]
+        }
+      ]
+    },
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Figures/Abadi et al. - 2024 - Hydrogeochemical characterization of groundwater in mountainous catchment and its suitability for dr/table_01.txt

@@ -0,0 +1 @@
+Descriptive statistics for the chemical analysis of groundwater samples (N ¼ 15) and classification of groundwater

Figures/Abadi et al. - 2024 - Hydrogeochemical characterization of groundwater in mountainous catchment and its suitability for dr/table_02.json

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Figures/Abadi et al. - 2024 - Hydrogeochemical characterization of groundwater in mountainous catchment and its suitability for dr/table_02.txt

@@ -0,0 +1 @@
+Hydrochemical facies of groundwater samples based on major ions (March 2020 samples)