{"id":18567,"date":"2015-06-02T18:01:25","date_gmt":"2015-06-02T18:01:25","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=18567"},"modified":"2015-06-03T12:40:03","modified_gmt":"2015-06-03T12:40:03","slug":"andres-and-blanca-in-the-eastern-pacific","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/18567","title":{"rendered":"Andres and Blanca in the eastern Pacific"},"content":{"rendered":"<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2015\/06\/GOES15_ANDRES_2JUNE2015anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2015\/06\/GOES15_ANDRES_2JUNE2015_1630.GIF\" alt=\"GOES-15 Imager 0.64 \u00b5m visible channel images (click to play animation)\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\"><strong>GOES-15 Imager 0.64 \u00b5m visible channel images<\/strong> (click to play animation)<\/p><\/div>\n<p>Hurricane Andres (above) in the eastern tropical Pacific was on 2 June 2015 joined by Tropical Storm Blanca (below).  Blanca was forecast to become a Hurricane later on 2 June as Andres weakens.  The circulation of Andres, above, is well-established, with good anti-cyclonic outflow and curved inflow bands.  <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2015\/06\/ANDRES_SHEAR_2June2015.gif\">Shear values<\/a> are low.  (Graphics come from <a href=\"http:\/\/tropic.ssec.wisc.edu\">this site<\/a>).  However, Andres has moved over relatively <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2015\/06\/ANDRES_SST_1200UTC_2June2015.gif\">cool Sea Surface Temperatures<\/a> that spell weakening.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2015\/06\/GOES15_BLANCA_2JUNE2015anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2015\/06\/GOES15_BLANCA_2JUNE2015_1630.GIF\" alt=\"GOES-15 Imager 0.64 \u00b5m visible channel images (click to play animation)\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\"><strong>GOES-15 Imager 0.64 \u00b5m visible channel images<\/strong> (click to play animation)<\/p><\/div>\n<p>Blanca, in contrast, has a circulation that is not so well-defined.  However, the storm <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2015\/06\/BLANCA_SST_2June2015.gif\">is over very warm water<\/a>, and also in a <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2015\/06\/SHEAR_BLANCA_2June2015.gif\">region of relatively low shear<\/a>.  Strengthening is forecast.<\/p>\n<p>The animation of Andres at top shows a ragged appearance as dry air intrudes upon the circulation from the south and west.  This dry air is apparent in the <a href=\"http:\/\/tropic.ssec.wisc.edu\/real-time\/mimic-tpw\/epac\/main.html\">MIMIC<\/a> Total Precipitable Water animation below.  The circulation of Blanca appears at the end of the animation, embedded within a rich source of tropical moisture.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2015\/06\/MIMIC_latest72hrs_ending2June2015.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2015\/06\/MIMIC_latest72hrs_ending2June2015.gif\" alt=\"3-day animation of MIMIC Total Precipitable Water over the eastern Pacific (click to enlarge)\" width=\"480\" height=\"220\" \/><\/a><p class=\"wp-caption-text\"><strong>3-day animation of MIMIC Total Precipitable Water over the eastern Pacific<\/strong> (click to enlarge)<\/p><\/div>\n<p>Sea-surface temperatures off the Pacific Coast of Mexico have been warmer than normal for much of this year (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2015\/06\/sstaanim_MarchToMay2015.gif\">Map<\/a>,  data from <a href=\"http:\/\/www.cpc.ncep.noaa.gov\/products\/analysis_monitoring\/enso_update\/sstanim.shtml\">here<\/a>).  Warmer-than-normal sea-surface temperatures argue for stronger hurricanes, and Andres was a <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2015\/06\/ANDRES_10.7_0900_01JUNE2015.GIF\">Category 4 storm on 1 June<\/a> with a well-developed eye.  Andres is one of only 5 May storms in the eastern Pacific since 1970 to achieve Major Hurricane status (<a href=\"http:\/\/www.nhc.noaa.gov\/archive\/2015\/ep01\/ep012015.discus.015.shtml?\">Link<\/a>).<\/p>\n<p>Aqua overflew Andres shortly before 1800 UTC on 1 June, and the water vapor imagery of the storm at that time is <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2015\/06\/ANDRES_WV_AQUA_1748_01June2015.gif\">here<\/a>.  The True-Color imagery is shown below.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a  href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2015\/06\/ANDRES_TRUECOLOR_AQUA_1748_01June2015.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2015\/06\/ANDRES_TRUECOLOR_AQUA_1748_01June2015.gif\" alt=\"Aqua True-Color Imagery, 1748 UTC on 1 June 2015 (click to enlarge)\" width=\"480\" height=\"420\" \/><\/a><p class=\"wp-caption-text\"><strong>Aqua True-Color Imagery, 1748 UTC on 1 June 2015 <\/Strong> (click to enlarge)<\/p><\/div>\n<p>A storm-centered animation over Andres&#8217; lifecycle is shown below.  The storm starts in the moisture-rich ITCZ and ends as an isolated region of moisture surrounded by dryness.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2015\/06\/GOES15_ANDRES_WV_SC_MAYJUNE2015_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2015\/06\/GOES15_ANDRES_WV_SC_MAYJUNE2015_17.GIF\" alt=\"GOES-15 Water Vapor Infrared Imagery (6.5\u00b5m) centered on Andres' center (click to animate)\" width=\"480\" height=\"340\" \/><\/a><p class=\"wp-caption-text\"><strong>GOES-15 Water Vapor Infrared Imagery (6.5\u00b5m) centered on Andres&#8217; center <\/Strong> (click to enlarge)<\/p><\/div>\n<p>For further information on these storms, consult the <a href=\"http:\/\/www.nhc.noaa.gov\">National Hurricane Center<\/a> website.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Hurricane Andres (above) in the eastern tropical Pacific was on 2 June 2015 joined by Tropical Storm Blanca (below). Blanca was forecast to become a Hurricane later on 2 June as Andres weakens. The circulation of Andres, above, is well-established, with good anti-cyclonic outflow and curved inflow bands. Shear values are low. (Graphics come from [&hellip;]<\/p>\n","protected":false},"author":19,"featured_media":18587,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[43,12,47,2],"tags":[],"class_list":["post-18567","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-15","category-modis","category-other-satellites","category-tropical-cyclones"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/18567","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/users\/19"}],"replies":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/comments?post=18567"}],"version-history":[{"count":23,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/18567\/revisions"}],"predecessor-version":[{"id":18592,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/18567\/revisions\/18592"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/18587"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=18567"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=18567"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=18567"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}