auto-update week 41

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Yo Robot 2025-10-07 15:00:25 +00:00
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commit 0a949deda7
254 changed files with 10791 additions and 12353 deletions

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@ -42,25 +42,25 @@
},
"Bathymetry": {
"continental shelf": {
"text": "the following are examples of features found on the continental shelf of the Southern Ocean (see Figure 2):<br><br>Astrid Ridge (see also Figure 4)<br>Belgrano Bank<br>Gunnerus Ridge (see also Figure 4)<br>Hayes Bank<br>Iselin Bank"
"text": "the following are examples of features on the continental shelf of the Southern Ocean (see Figure 2):<br><br>Astrid Ridge (see also Figure 4)<br>Belgrano Bank<br>Gunnerus Ridge (see also Figure 4)<br>Hayes Bank<br>Iselin Bank"
},
"continental slope": {
"text": "the following are examples of features found on the continental slope of the Southern Ocean (see Figure 2):<br><br>Amery Basin (Figure 4)<br>Filchner Trough<br>Hillary Canyon<br>Pobeda Canyon (Figure 3)"
"text": "the following are examples of features on the continental slope of the Southern Ocean (see Figure 2):<br><br>Amery Basin (Figure 4)<br>Filchner Trough<br>Hillary Canyon<br>Pobeda Canyon (Figure 3)"
},
"abyssal plains": {
"text": "the following are examples of features found on the abyssal plains of the Southern Ocean (see Figures 2, 3, and 4):<br><br>Amundsen (Abyssal) Plain<br>Enderby (Abyssal) Plain<br>South Indian/Australian-Antarctic Basin<br>Southeast Pacific/Bellinghausen Basin<br>Weddell (Abyssal) Plain"
"text": "the following are examples of features on the abyssal plains of the Southern Ocean (see Figures 2, 3, and 4):<br><br>Amundsen (Abyssal) Plain<br>Enderby (Abyssal) Plain<br>South Indian/Australian-Antarctic Basin<br>Southeast Pacific/Bellinghausen Basin<br>Weddell (Abyssal) Plain"
},
"mid-ocean ridge": {
"text": "the following are examples of mid-ocean ridges found on the floor of the Southern Ocean (see Figure 2):<br><br>Pacific-Antarctic Ridge (Figure 3)"
"text": "the following are examples of mid-ocean ridges on the floor of the Southern Ocean (see Figure 2):<br><br>Pacific-Antarctic Ridge (Figure 3)"
},
"undersea terrain features": {
"text": "the following are examples of undersea terrain features found on the floor of the Southern Ocean (see Figure 2):<br><br>Akopov Seamounts (Figure 3)<br>De Gerlache Seamounts (see also Figure 3, 4)<br>Endurance Ridge (Figure 4)<br>Marie Byrd Seamount (see also Figure 3)<br>Maud Rise (see also Figure 4)<br>Scott Seamounts (see also Figure 3)"
"text": "the following are examples of undersea terrain features on the floor of the Southern Ocean (see Figure 2):<br><br>Akopov Seamounts (Figure 3)<br>De Gerlache Seamounts (see also Figure 3, 4)<br>Endurance Ridge (Figure 4)<br>Marie Byrd Seamount (see also Figure 3)<br>Maud Rise (see also Figure 4)<br>Scott Seamounts (see also Figure 3)"
},
"ocean trenches": {
"text": "<p>the following are examples of ocean trenches found on the floor of the Southern Ocean (see Figure 2):<br><br>South Sandwich Trench (Figure 4; the deepest location in the Southern Ocean)</p>"
"text": "the following are examples of ocean trenches on the floor of the Southern Ocean (see Figure 2):<br><br>South Sandwich Trench (Figure 4; the deepest location in the Southern Ocean)"
},
"atolls": {
"text": "due to the extremely cold water, there are no atolls in the Southern Ocean"
"text": "none, due to the extremely cold water"
}
},
"Elevation": {
@ -87,8 +87,6 @@
"text": "the major chokepoint is the Drake Passage between South America and Antarctica; the Polar Front (Antarctic Convergence) is the best natural definition of the northern extent of the Southern Ocean; it is a distinct region at the middle of the Antarctic Circumpolar Current that separates the cold polar surface waters to the south from the warmer waters to the north; the Front and the Current extend entirely around Antarctica, reaching south of 60 degrees south near New Zealand and near 48 degrees south in the far South Atlantic, coinciding with the path of the maximum westerly winds"
}
},
"People and Society": {
},
"Environment": {
"Environmental issues": {
"text": "natural and man-made changes to the ocean's physical, chemical, and biological systems&nbsp;"