{"id":50267,"date":"2023-02-05T09:54:00","date_gmt":"2023-02-05T09:54:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=50267"},"modified":"2023-02-07T20:18:51","modified_gmt":"2023-02-07T20:18:51","slug":"sentinel-1a-sar-data-over-the-south-pacific","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/50267","title":{"rendered":"Sentinel 1A SAR data over the South Pacific"},"content":{"rendered":"\n
\"\"<\/a>
Sentinel 1A Derived Wind Speed and Normalized Radar Cross Section, 06:00:18 on 5 February 2023 (click to enlarge)<\/figcaption><\/figure>\n\n\n\n

As noted previously, NOAA\/STAR has arranged for special Synthetic Aperture Radar (SAR) wind observations over American Samoa during the month of February. Sentinel-1A SAR also provides occasional observations in and around the Samoan islands. The toggle above compares (using imagery from this website<\/a>) derived wind speed<\/a> and Normalized Radar Cross Section (NRCS)<\/a> at 0600 UTC on 5 February 2023; a corresponding GOES-18 Clean Window infrared image is shown below, with the western-most end of a convective feature sampled (Here is the image<\/a> without the sampling information). The coldest brightness temperatures with that convective complex are in the -61 to -66o<\/sup>C range. (This animation from 0500 to 0750 UTC<\/a> shows the convection decaying with time).<\/p>\n\n\n\n

\"\"
GOES-18 Clean Window infrared (10.3 \u00b5m) imagery, 0600 UTC on 5 February 2023 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n

Outflow winds with this system are in the 15-20 knot range (bright cyan colors). The strongest derived winds — along 15.4o N in the wind analysis — are a result of ice in the cloud affecting the cloud signal. The NRCS for that region has the feathery characteristic of highly reflective ice crystals.<\/p>\n\n\n\n

\"\"<\/a>
Sentinel 1A Derived winds (left) and Normalized Radar Cross Section (NRCS) (right), both at 0600 UTC on 5 February 2023 (click to enlarge)<\/figcaption><\/figure>\n\n\n\n

Sentinel-1A continued north, and sampled the waters surrounding Samoa, as shown in the toggle of derived windspeed<\/a> and NRCS<\/a> below. The island of Savai’i has an affect on the winds!<\/p>\n\n\n\n

\"\"<\/a>
Derived Winds and Normalized Radar Cross Section (NRCS) at 06:00:44 on 5 February 2023 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n
\n\n\n\n

When comparing SAR surface winds and GOES-18 (or any geostationary satellite) imagery, you must make sure to consider the effects of parallax. The satellite information may be parallax-shifted. Thus, the coldest brightness temperatures in the ABI imagery may not align with the region where ice crystals are affecting the SAR signal.<\/p>\n\n\n\n

\"\"
GOES-18 Clean Window infrared (10.3 \u00b5m) imagery and Sentinel 1A SAR Winds, 0600 UTC on 5 February 2023 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n

<\/p>\n","protected":false},"excerpt":{"rendered":"

As noted previously, NOAA\/STAR has arranged for special Synthetic Aperture Radar (SAR) wind observations over American Samoa during the month of February. Sentinel-1A SAR also provides occasional observations in and around the Samoan islands. The toggle above compares (using imagery from this website) derived wind speed and Normalized Radar Cross Section (NRCS) at 0600 UTC […]<\/p>\n","protected":false},"author":19,"featured_media":50271,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[114,104,25],"tags":[],"class_list":["post-50267","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-18","category-sar","category-satellite-winds"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/50267","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=50267"}],"version-history":[{"count":7,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/50267\/revisions"}],"predecessor-version":[{"id":50306,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/50267\/revisions\/50306"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/50271"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=50267"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=50267"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=50267"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}