{"id":45831,"date":"2022-04-19T17:25:15","date_gmt":"2022-04-19T17:25:15","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=45831"},"modified":"2022-04-19T17:25:15","modified_gmt":"2022-04-19T17:25:15","slug":"nucaps-fields-over-american-samoa","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/45831","title":{"rendered":"NUCAPS fields over American Samoa"},"content":{"rendered":"\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"904\" height=\"482\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/04\/SoundingAvailabilityZoom-20220419_130359.png\" alt=\"\" class=\"wp-image-45832\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/04\/SoundingAvailabilityZoom-20220419_130359.png 904w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/04\/SoundingAvailabilityZoom-20220419_130359-300x160.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/04\/SoundingAvailabilityZoom-20220419_130359-768x409.png 768w\" sizes=\"auto, (max-width: 904px) 100vw, 904px\" \/><figcaption>Sounding Availability fields over the South Pacific, 1234 UTC on 19 April 2022.  Note the two green dots to the north and south of American Samoa (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>Oceans such as the South Pacific can be a large data void.  NOAA-20 NUCAPS profiles can be an important data source to define the state of the atmosphere.  The image above shows NUCAPS Sounding Availability from the overnight pass over American Samoa; the largest island of American Samoa, Tutuila, is just west of 170<sup>o<\/sup>W in image above.  There are green circles just north and just south of Tutuila, signifying locations of NUCAPS profiles associated with successful retrievals.  The toggle below compares those two profiles with the 1200 UTC rawinsonde launch (NSTU) from Pago Pago.  Good agreement is apparent, although the NUCAPS profiles are smoother.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"669\" height=\"338\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/04\/NUCAPSProfile_NSTUSounding_1200_19April2022.gif\" alt=\"\" class=\"wp-image-45833\" \/><figcaption>NUCAPS soundings just north and south of American Samoa (1308 UTC), and the 1200 UTC Radiosonde at NSTU, 19 April 2022 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>The environment is somewhat dry.  This is confirmed by a MIMIC Total Precipitable water mapping, shown below (for 1200 UTC on 19 April 2022) in an image taken from <a href=\"http:\/\/tropic.ssec.wisc.edu\/real-time\/mtpw2\/product.php?color_type=tpw_nrl_colors&amp;prod=spac&amp;timespan=24hrs&amp;anim=html5\">here<\/a>.  The Samoan islands are between two bands of moisture.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"1000\" height=\"470\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/04\/MIMICTPW2_1200UTC_19April2022.png\" alt=\"\" class=\"wp-image-45834\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/04\/MIMICTPW2_1200UTC_19April2022.png 1000w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/04\/MIMICTPW2_1200UTC_19April2022-300x141.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/04\/MIMICTPW2_1200UTC_19April2022-768x361.png 768w\" sizes=\"auto, (max-width: 1000px) 100vw, 1000px\" \/><figcaption>MIMIC Total Precipitable Water, 1200 UTC on 19 April 2022<\/figcaption><\/figure>\n\n\n\n<p>NUCAPS profiles give useful information, but it can be cumbersome to view all individual profiles sequentially.  Gridded fields of various properties are available in AWIPS (and online <a href=\"https:\/\/weather.msfc.nasa.gov\/cgi-bin\/sportPublishData.pl?dataset=griddednucaps&amp;product=web14d_LR850.png&amp;stamp=20220419_1214&amp;loc=spacific#image\">here<\/a> and <a href=\"https:\/\/nucaps.ssec.wisc.edu\">here<\/a>).  The toggle below shows a larger view than the topmost image, and it compares gridded Temperature fields at 950 mb, and the 950-700 mb lapse rate.  Over the Samoan islands, 950-mb temperatures are faily uniform around 23<sup>o<\/sup> C, with &#8220;cooler&#8221; temperatures (closer to 21<sup>o<\/sup> C) just to the northeast.  Lapse rates are stable: between 4 and 5 <sup>o<\/sup>C\/km.  As you might expect given the relative dryness and stability, shower chances over American Samoa for 19 April are low.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/04\/SoundingAvail_T950_LR950-700-20220419_1303toggle.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"904\" height=\"482\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/04\/SoundingAvail_T950_LR950-700-20220419_1303toggle.gif\" alt=\"\" class=\"wp-image-45835\" \/><\/a><figcaption>NUCAPS Soundings Availability points over the South Pacific, along with gridded fields of 950-mb Temperature, and 950-700mb Lapse Rates (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>Use NUCAPS when your weather is approaching from a region void of conventional data.<\/p>\n\n\n\n<hr class=\"wp-block-separator\" \/>\n\n\n\n<p>Imagery in this blog post was in part from the NOAA\/TOWR-S instance of AWIPS in the Cloud.  Thank you!<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Oceans such as the South Pacific can be a large data void. NOAA-20 NUCAPS profiles can be an important data source to define the state of the atmosphere. The image above shows NUCAPS Sounding Availability from the overnight pass over American Samoa; the largest island of American Samoa, Tutuila, is just west of 170oW in [&hellip;]<\/p>\n","protected":false},"author":19,"featured_media":45835,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[78,83],"tags":[],"class_list":["post-45831","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-noaa-20","category-nucaps"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/45831","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=45831"}],"version-history":[{"count":2,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/45831\/revisions"}],"predecessor-version":[{"id":45837,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/45831\/revisions\/45837"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/45835"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=45831"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=45831"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=45831"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}