{"id":3874,"date":"2021-02-28T11:03:37","date_gmt":"2021-02-28T11:03:37","guid":{"rendered":"http:\/\/thales.mit.edu\/bush\/?page_id=3874"},"modified":"2021-04-15T00:44:17","modified_gmt":"2021-04-15T00:44:17","slug":"geophysical-flows","status":"publish","type":"page","link":"https:\/\/thales.mit.edu\/bush\/index.php\/geophysical-flows\/","title":{"rendered":"Geophysical flows"},"content":{"rendered":"\n<div class=\"wp-block-cover alignwide has-subtle-background-color has-background-dim is-style-twentytwentyone-border\" style=\"min-height:188px;aspect-ratio:unset;\"><div class=\"wp-block-cover__inner-container is-layout-flow wp-block-cover-is-layout-flow\">\n<h3 class=\"has-text-align-center wp-block-heading\">Geophysical flows<\/h3>\n\n\n\n<p class=\"has-text-align-left has-normal-font-size\">Some of my early work concerned the dynamics of large scale flows dominated by the influence of stratification and the Earth\u2019s rotation, as arise in the Earth\u2019s atmosphere and oceans. Other geophysical research subjects have included the dynamics of tektites, the dynamics of the Earth\u2019s lithosphere, and the dynamics of sedimentation, as arises in the world\u2019s rivers and lakes.&nbsp;<\/p>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-group alignfull\"><div class=\"wp-block-group__inner-container is-layout-flow wp-block-group-is-layout-flow\"><ul class=\"wp-block-latest-posts__list is-grid columns-5 alignwide tw-heading-size-small tw-stretched-link is-style-twentytwentyone-latest-posts-dividers tw-img-ratio-1-1 wp-block-latest-posts\"><li><div class=\"wp-block-latest-posts__featured-image\"><img loading=\"lazy\" decoding=\"async\" width=\"300\" height=\"156\" src=\"https:\/\/thales.mit.edu\/bush\/wp-content\/uploads\/2021\/03\/wave-break-300x156-1.jpg\" class=\"attachment-large size-large wp-post-image\" alt=\"\" style=\"width:100%;height:52%;max-width:300px;\" \/><\/div><a class=\"wp-block-latest-posts__post-title\" href=\"https:\/\/thales.mit.edu\/bush\/index.php\/2021\/04\/15\/drops-and-bubbles-in-the-environment\/\">Drops and bubbles in the environment<\/a><\/li>\n<li><div class=\"wp-block-latest-posts__featured-image\"><img loading=\"lazy\" decoding=\"async\" width=\"409\" height=\"301\" src=\"https:\/\/thales.mit.edu\/bush\/wp-content\/uploads\/2012\/09\/Clarke-Bush2.jpg\" class=\"attachment-large size-large wp-post-image\" alt=\"\" style=\"width:100%;height:73.59%;max-width:409px;\" \/><\/div><a class=\"wp-block-latest-posts__post-title\" href=\"https:\/\/thales.mit.edu\/bush\/index.php\/2009\/04\/14\/the-drainage-of-glacial-lakes-and-climate-change\/\">The drainage of glacial lakes<\/a><\/li>\n<li><div class=\"wp-block-latest-posts__featured-image\"><img loading=\"lazy\" decoding=\"async\" width=\"390\" height=\"356\" src=\"https:\/\/thales.mit.edu\/bush\/wp-content\/uploads\/2021\/04\/Bosak-thumb.png\" class=\"attachment-large size-large wp-post-image\" alt=\"\" style=\"width:100%;height:91.28%;max-width:390px;\" \/><\/div><a class=\"wp-block-latest-posts__post-title\" href=\"https:\/\/thales.mit.edu\/bush\/index.php\/2009\/04\/14\/formation-and-stability-of-oxygen-rich-bubbles-that-shape-photosynthetic-mats\/\">Bubbles that shape photosynthetic mats<\/a><\/li>\n<li><div class=\"wp-block-latest-posts__featured-image\"><img loading=\"lazy\" decoding=\"async\" width=\"284\" height=\"252\" src=\"https:\/\/thales.mit.edu\/bush\/wp-content\/uploads\/2021\/03\/rollwaves2-thumb.png\" class=\"attachment-large size-large wp-post-image\" alt=\"\" style=\"width:100%;height:88.73%;max-width:284px;\" \/><\/div><a class=\"wp-block-latest-posts__post-title\" href=\"https:\/\/thales.mit.edu\/bush\/index.php\/2005\/04\/14\/roll-waves-on-flowing-cornstarch-suspensions\/\">Roll waves on flowing cornstarch<\/a><\/li>\n<li><div class=\"wp-block-latest-posts__featured-image\"><img loading=\"lazy\" decoding=\"async\" width=\"1000\" height=\"899\" src=\"https:\/\/thales.mit.edu\/bush\/wp-content\/uploads\/2021\/03\/Tibet-thumb-1.png\" class=\"attachment-large size-large wp-post-image\" alt=\"\" style=\"width:100%;height:89.94%;max-width:1074px;\" \/><\/div><a class=\"wp-block-latest-posts__post-title\" href=\"https:\/\/thales.mit.edu\/bush\/index.php\/2005\/04\/14\/the-dynamics-of-the-tibetan-plateau\/\">The dynamics of the Tibetan Plateau<\/a><\/li>\n<li><div class=\"wp-block-latest-posts__featured-image\"><img loading=\"lazy\" decoding=\"async\" width=\"474\" height=\"438\" src=\"https:\/\/thales.mit.edu\/bush\/wp-content\/uploads\/2021\/03\/tektite-thumb.png\" class=\"attachment-large size-large wp-post-image\" alt=\"\" style=\"width:100%;height:92.41%;max-width:474px;\" \/><\/div><a class=\"wp-block-latest-posts__post-title\" href=\"https:\/\/thales.mit.edu\/bush\/index.php\/2003\/04\/14\/the-dynamics-of-splash-form-tektites\/\">The dynamics of splash-form tektites<\/a><\/li>\n<li><div class=\"wp-block-latest-posts__featured-image\"><img loading=\"lazy\" decoding=\"async\" width=\"550\" height=\"512\" src=\"https:\/\/thales.mit.edu\/bush\/wp-content\/uploads\/2021\/03\/ParticlePlume-thumb.png\" class=\"attachment-large size-large wp-post-image\" alt=\"\" style=\"width:100%;height:93.09%;max-width:550px;\" \/><\/div><a class=\"wp-block-latest-posts__post-title\" href=\"https:\/\/thales.mit.edu\/bush\/index.php\/2003\/03\/20\/sedimentation-from-particle-clouds\/\">Sedimentation from particle clouds<\/a><\/li>\n<li><div class=\"wp-block-latest-posts__featured-image\"><img loading=\"lazy\" decoding=\"async\" width=\"560\" height=\"552\" src=\"https:\/\/thales.mit.edu\/bush\/wp-content\/uploads\/2021\/03\/Sed-river-thumb-1.png\" class=\"attachment-large size-large wp-post-image\" alt=\"\" style=\"width:100%;height:98.57%;max-width:560px;\" \/><\/div><a class=\"wp-block-latest-posts__post-title\" href=\"https:\/\/thales.mit.edu\/bush\/index.php\/2001\/03\/20\/sedimentation-from-riverine-outflows\/\">Sedimentation from riverine outflows<\/a><\/li>\n<li><div class=\"wp-block-latest-posts__featured-image\"><img loading=\"lazy\" decoding=\"async\" width=\"604\" height=\"558\" src=\"https:\/\/thales.mit.edu\/bush\/wp-content\/uploads\/2021\/03\/vortices-thumb.png\" class=\"attachment-large size-large wp-post-image\" alt=\"\" style=\"width:100%;height:92.38%;max-width:604px;\" \/><\/div><a class=\"wp-block-latest-posts__post-title\" href=\"https:\/\/thales.mit.edu\/bush\/index.php\/2000\/04\/14\/line-plumes-in-rotation-leads-and-megaplumes\/\">Line plumes in rotation<\/a><\/li>\n<li><div class=\"wp-block-latest-posts__featured-image\"><img loading=\"lazy\" decoding=\"async\" width=\"372\" height=\"392\" src=\"https:\/\/thales.mit.edu\/bush\/wp-content\/uploads\/2021\/03\/reddrop-thumb.png\" class=\"attachment-large size-large wp-post-image\" alt=\"\" style=\"width:100%;height:105.38%;max-width:372px;\" \/><\/div><a class=\"wp-block-latest-posts__post-title\" href=\"https:\/\/thales.mit.edu\/bush\/index.php\/1993\/04\/14\/drop-motion-in-rapidly-rotating-flows\/\">Drop motion in rapidly rotating flows<\/a><\/li>\n<\/ul><\/div><\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"--col-width:100%;flex-basis:100%\">\n<div class=\"wp-block-group is-layout-flow wp-block-group-is-layout-flow\"><div class=\"wp-block-group__inner-container\"><\/div><\/div>\n<\/div>\n<\/div>\n","protected":false},"excerpt":{"rendered":"","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"tw-no-title.php","meta":{"footnotes":""},"class_list":["post-3874","page","type-page","status-publish","hentry","entry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v16.3 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Geophysical flows - John W. 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