div class=ts-pagebutton class=gotoPage data-page=1Page 1button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=1 data-page=1 class=ts-thumb lazyload alt=Page 1: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails1jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=2Page 2button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=2 data-page=2 class=ts-thumb lazyload alt=Page 2: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails2jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=3Page 3button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=3 data-page=3 class=ts-thumb lazyload alt=Page 3: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails3jpg width=140 height=200 divdivdiv 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Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails5jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=6Page 6button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=6 data-page=6 class=ts-thumb lazyload alt=Page 6: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails6jpg width=140 height=200 divdivdiv 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Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails8jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=9Page 9button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=9 data-page=9 class=ts-thumb lazyload alt=Page 9: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails9jpg width=140 height=200 divdivdiv 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develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails11jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=12Page 12button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=12 data-page=12 class=ts-thumb lazyload alt=Page 12: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails12jpg width=140 height=200 divdivdiv 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develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails14jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=15Page 15button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=15 data-page=15 class=ts-thumb lazyload alt=Page 15: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails15jpg width=140 height=200 divdivdiv 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develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails17jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=18Page 18button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=18 data-page=18 class=ts-thumb lazyload alt=Page 18: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails18jpg width=140 height=200 divdivdiv 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develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails20jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=21Page 21button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=21 data-page=21 class=ts-thumb lazyload alt=Page 21: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails21jpg width=140 height=200 divdivdiv 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develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails23jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=24Page 24button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=24 data-page=24 class=ts-thumb lazyload alt=Page 24: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails24jpg width=140 height=200 divdivdiv 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develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails26jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=27Page 27button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=27 data-page=27 class=ts-thumb lazyload alt=Page 27: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails27jpg width=140 height=200 divdivdiv 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develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails29jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=30Page 30button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=30 data-page=30 class=ts-thumb lazyload alt=Page 30: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails30jpg width=140 height=200 divdivdiv 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develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails32jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=33Page 33button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=33 data-page=33 class=ts-thumb lazyload alt=Page 33: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails33jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=34Page 34button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=34 data-page=34 class=ts-thumb lazyload alt=Page 34: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails34jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=35Page 35button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=35 data-page=35 class=ts-thumb lazyload alt=Page 35: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails35jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=36Page 36button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=36 data-page=36 class=ts-thumb lazyload alt=Page 36: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails36jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=37Page 37button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=37 data-page=37 class=ts-thumb lazyload alt=Page 37: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails37jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=38Page 38button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=38 data-page=38 class=ts-thumb lazyload alt=Page 38: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails38jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=39Page 39button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=39 data-page=39 class=ts-thumb lazyload alt=Page 39: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails39jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=40Page 40button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=40 data-page=40 class=ts-thumb lazyload alt=Page 40: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails40jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=41Page 41button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=41 data-page=41 class=ts-thumb lazyload alt=Page 41: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails41jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=42Page 42button div class=ts-imageimg data-url=earth-peltier-gradient-richardson-number-at-co-and-r3-linear-stabilityhtmlpage=42 data-page=42 class=ts-thumb lazyload alt=Page 42: Earthpeltier · gradient Richardson number at C=O and R=3 Linear stability theory predicts that the flow will develop Holmboe instability when J exceeds some critical value J loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader035vdocumentinreader035viewer20220710135fcb81bd6c8eee009c28e44dhtml5thumbnails42jpg width=140 height=200 divdiv
