{"id":2419,"date":"2015-01-13T11:40:08","date_gmt":"2015-01-13T18:40:08","guid":{"rendered":"http:\/\/rammb.cira.colostate.edu\/projects\/npp\/blog\/?p=2419"},"modified":"2026-03-06T17:36:40","modified_gmt":"2026-03-06T17:36:40","slug":"sea-effect-snow","status":"publish","type":"post","link":"https:\/\/rammb2.cira.colostate.edu\/npp-blog\/2015\/01\/13\/sea-effect-snow\/","title":{"rendered":"Sea-effect Snow"},"content":{"rendered":"\n<p>Take a look at this image:<\/p>\n\n\n\n<figure class=\"wp-block-image\"><a href=\"https:\/\/rammb2.cira.colostate.edu\/jpss-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/10898316_1620763321480096_8641670430677468225_n.jpg\"><img loading=\"lazy\" decoding=\"async\" width=\"720\" height=\"960\" src=\"https:\/\/rammb2.cira.colostate.edu\/jpss-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/10898316_1620763321480096_8641670430677468225_n.jpg\" alt=\"Photo credit: \u0130skender \u015eeng\u00f6r via Severe Weather Europe on Facebook\" class=\"wp-image-2422\" srcset=\"https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/10898316_1620763321480096_8641670430677468225_n.jpg 720w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/10898316_1620763321480096_8641670430677468225_n-225x300.jpg 225w\" sizes=\"auto, (max-width: 720px) 100vw, 720px\" \/><\/a><figcaption class=\"wp-element-caption\">Photo credit: \u0130skender \u015eeng\u00f6r via Severe Weather Europe on Facebook<\/figcaption><\/figure>\n\n\n\n<p>Is this picture from A) the <a href=\"http:\/\/en.wikipedia.org\/wiki\/Keweenaw_Peninsula#mediaviewer\/File:Keweenaw_Snow_Thermometer.jpg\" target=\"_blank\" rel=\"noopener\">Keweenaw Peninsula of Michigan in 1978<\/a>? B) <a href=\"http:\/\/kdvr.com\/2014\/11\/19\/snowvember-buffalos-best-social-media-posts-of-historic-snowfall\/\" target=\"_blank\" rel=\"noopener\">Orchard Park, New York in November 2014 (aka &#8220;Snowvember&#8221;)<\/a>? or C) <a href=\"http:\/\/en.wikipedia.org\/wiki\/%C4%B0nebolu\" target=\"_blank\" rel=\"noopener\">\u0130nebolu, Turkey<\/a> from just last week?<\/p>\n\n\n\n<p>If you pay attention to details, you will have noticed that I credited \u0130skender \u015eeng\u00f6r with the picture and properly surmised that the answer is C. If you don&#8217;t pay attention to details, get off my blog! The details are where all the interesting stuff happens! You&#8217;d never be able to <a href=\"https:\/\/rammb.cira.colostate.edu\/projects\/npp\/blog\/index.php\/uncategorized\/wild-week-of-wildfires-part-iii\/\" target=\"_blank\" rel=\"noopener\">identify small fires<\/a> or <a href=\"https:\/\/rammb.cira.colostate.edu\/projects\/npp\/blog\/index.php\/uncategorized\/aurora-australis-from-the-day-night-band\/\" target=\"_blank\" rel=\"noopener\">calculate the speed of an aurora<\/a>&nbsp; or <a href=\"https:\/\/rammb.cira.colostate.edu\/projects\/npp\/blog\/index.php\/uncategorized\/investigating-mysteries-of-the-deep-dark-night\/\" target=\"_blank\" rel=\"noopener\">explain the unknown<\/a> without paying attention to details.<\/p>\n\n\n\n<p>If you follow the weather (or social media), you probably know about lake-effect snow. (Who can forget <a href=\"http:\/\/www.buffalonews.com\/city-region\/weather\/were-calling-this-one-snowvember-20141122\" target=\"_blank\" rel=\"noopener\">Snowvember<\/a>?) But, have you heard of sea-effect snow?<\/p>\n\n\n\n<p>Areas downwind of the Great Lakes get a lot more snow than areas upwind of the Lakes. I was going to explain why in great detail, but <a href=\"http:\/\/www.weather5280.com\/blog\/2014\/11\/25\/lake-effect-snow-explained\/\" target=\"_blank\" rel=\"noopener\">this guy saved me a lot of time and effort<\/a>. (I have since been notified that much of the material in that last link was lifted from a <a href=\"https:\/\/rammb.cira.colostate.edu\/training\/visit\/training_sessions\/\" target=\"_blank\" rel=\"noopener\">VISIT Training Session<\/a> put together by our very own Dan B. You can watch and listen to that training session <a href=\"https:\/\/rammb.cira.colostate.edu\/training\/visit\/training_sessions\/lake-effect_snow_1\/video\/\" target=\"_blank\" rel=\"noopener\">here<\/a>.) The physical processes that cause lake-effect snow are not limited to the Great Lakes, however. Anywhere you have a large body of relatively warm water (meaning it doesn&#8217;t <a href=\"https:\/\/rammb.cira.colostate.edu\/projects\/npp\/blog\/index.php\/uncategorized\/hell-froze-over-and-the-great-lakes-too\/\" target=\"_blank\" rel=\"noopener\">freeze over<\/a>) with episodes of very cold winds in the winter you get lake-effect or sea-effect snow.<\/p>\n\n\n\n<p>When you think of the great snowbelts of the world, you probably don&#8217;t think of Turkey &#8211; but you should! Arctic air outbreaks associated with strong northerly winds blowing across the Black Sea can generate snow at the same rate as Snowvember or <a href=\"http:\/\/en.wikipedia.org\/wiki\/Snowmageddon\" target=\"_blank\" rel=\"noopener\">Snowpocalypse or Snowmageddon<\/a> or any other silly name that the media can come up with that has &#8220;snow&#8221; in it (Snowbruary, Snowtergate aka Frozen-Watergate, Snowlloween, Martin Luther Snow Day, Snowco de Mayo, Snowth of July&#8230; Just remember, I coined all of these phrases if you hear them later). Plus, the <a href=\"http:\/\/en.wikipedia.org\/wiki\/Pontic_Mountains\" target=\"_blank\" rel=\"noopener\">Pontic Mountains<\/a> provide a greater upslope enhancement than the <a href=\"http:\/\/wasatchweatherweenies.blogspot.com\/2013\/10\/the-owles-field-program-adventures-on.html\" target=\"_blank\" rel=\"noopener\">Tug Hill Plateau<\/a> in Upstate New York.<\/p>\n\n\n\n<p>One such Arctic outbreak occurred from 7-9 January 2015, resulting in the picture above. Parts of Turkey received 2 meters (!) of snow (78 inches to Americans) in a 2-3 day period, as if you couldn&#8217;t tell from that picture or <a href=\"https:\/\/www.facebook.com\/severeweatherEU\/photos\/a.1423656947857402.1073741825.1377757209114043\/1620762004813561\/?type=1&amp;theater\" target=\"_blank\" rel=\"noopener\">this one<\/a>.<\/p>\n\n\n\n<p>From satellites, sea-effect snow looks just like lake-effect snow. (Duh! It&#8217;s the same physical process!) Here&#8217;s a VIIRS &#8220;True Color&#8221; image of the lake-effect snow event that took place last week on the Great Lakes:<\/p>\n\n\n\n<figure class=\"wp-block-image\"><a href=\"https:\/\/rammb2.cira.colostate.edu\/jpss-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M03_M04_M05_20150107_1924384_1927279_rayleigh_log.png\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"987\" src=\"https:\/\/rammb2.cira.colostate.edu\/jpss-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M03_M04_M05_20150107_1924384_1927279_rayleigh_log-1024x987.png\" alt=\"VIIRS &quot;True Color&quot; RGB composite, taken 19:24 UTC 7 January 2015\" class=\"wp-image-2431\" srcset=\"https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M03_M04_M05_20150107_1924384_1927279_rayleigh_log-1024x987.png 1024w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M03_M04_M05_20150107_1924384_1927279_rayleigh_log-300x289.png 300w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M03_M04_M05_20150107_1924384_1927279_rayleigh_log-768x740.png 768w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M03_M04_M05_20150107_1924384_1927279_rayleigh_log-1536x1481.png 1536w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M03_M04_M05_20150107_1924384_1927279_rayleigh_log-2048x1975.png 2048w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption class=\"wp-element-caption\">VIIRS &#8220;True Color&#8221; RGB composite, taken 19:24 UTC 7 January 2015.<\/figcaption><\/figure>\n\n\n\n<p>Wait &#8211; that&#8217;s no good! We need to be able to distinguish the snow from the clouds. Let&#8217;s try that again with the &#8220;<a href=\"https:\/\/rammb.cira.colostate.edu\/projects\/npp\/blog\/index.php\/uncategorized\/end-of-autumn-in-the-alps\/\" target=\"_blank\" rel=\"noopener\">Natural Color<\/a>&#8221; RGB composite:<\/p>\n\n\n\n<figure class=\"wp-block-image\"><a href=\"https:\/\/rammb2.cira.colostate.edu\/jpss-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150107_1924384_1927279.png\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"987\" src=\"https:\/\/rammb2.cira.colostate.edu\/jpss-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150107_1924384_1927279-1024x987.png\" alt=\"VIIRS &quot;Natural Color&quot; RGB composite, taken 19:24 UTC 7 January 2015\" class=\"wp-image-2432\" srcset=\"https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150107_1924384_1927279-1024x987.png 1024w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150107_1924384_1927279-300x289.png 300w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150107_1924384_1927279-768x740.png 768w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150107_1924384_1927279-1536x1481.png 1536w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150107_1924384_1927279-2048x1975.png 2048w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption class=\"wp-element-caption\">VIIRS &#8220;Natural Color&#8221; RGB composite, taken 19:24 UTC 7 January 2015.<\/figcaption><\/figure>\n\n\n\n<p>That&#8217;s better. Notice how the clouds are formed right over the lakes and how the clouds organize themselves into bands called &#8220;<a href=\"http:\/\/earthsky.org\/earth\/what-are-cloud-streets\" target=\"_blank\" rel=\"noopener\">cloud streets<\/a>&#8220;. The same features are visible in the sea-effect snow event over Turkey (from one day later):<\/p>\n\n\n\n<figure class=\"wp-block-image\"><a href=\"https:\/\/rammb2.cira.colostate.edu\/jpss-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150108_1036273_1040423.png\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"698\" src=\"https:\/\/rammb2.cira.colostate.edu\/jpss-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150108_1036273_1040423-1024x698.png\" alt=\"VIIRS &quot;Natural Color&quot; RGB composite, taken 10:36 UTC 8 January 2015\" class=\"wp-image-2433\" srcset=\"https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150108_1036273_1040423-1024x698.png 1024w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150108_1036273_1040423-300x205.png 300w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150108_1036273_1040423-768x524.png 768w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150108_1036273_1040423-1536x1047.png 1536w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150108_1036273_1040423-2048x1396.png 2048w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption class=\"wp-element-caption\">VIIRS &#8220;Natural Color&#8221; RGB composite, taken 10:36 UTC 8 January 2015.<\/figcaption><\/figure>\n\n\n\n<p>Look at how much of Turkey is covered by snow! (Most of that snow cover is from the low pressure system that passed over Turkey a couple days before the sea-effect snow machine kicked in.) And &#8211; *cough* attention to details *cough* &#8211; you can even see snow over Greece and more sea-effect snow on Crete. There&#8217;s also snow down in Syria, Lebanon and Israel (Israel is off the bottom of the image), which is <a href=\"http:\/\/www.bbc.co.uk\/weather\/features\/30717219\" target=\"_blank\" rel=\"noopener\">bad news for Syrian refugees<\/a>.The heavy snow has <a href=\"http:\/\/www.todayszaman.com\/national_heavy-snowfall-continues-to-paralyze-turkey_369176.html\" target=\"_blank\" rel=\"noopener\">shut down thousands of roads, closed schools and businesses<\/a>, and was even the source of a <a href=\"http:\/\/www.bbc.com\/news\/blogs-news-from-elsewhere-30696997\" target=\"_blank\" rel=\"noopener\">political scandal<\/a>.<\/p>\n\n\n\n<p>But, on the plus side, the Arctic outbreak in the Middle East brings a unique opportunity to see <a href=\"http:\/\/www.theweathernetwork.com\/news\/articles\/snow-blankets-the-middle-east-as-rare-winter-storm-affects-area\/43170\/\" target=\"_blank\" rel=\"noopener\">palm trees covered in snow<\/a>. And, how often do you get to see the <a href=\"https:\/\/www.facebook.com\/severeweatherEU\/photos\/a.1423656947857402.1073741825.1377757209114043\/1621711441385284\/?type=1&amp;theater\" target=\"_blank\" rel=\"noopener\">deserts of Saudi Arabia covered in snow<\/a>? (EUMETSAT has provided more satellite images of this event at their <a href=\"http:\/\/www.eumetsat.int\/website\/home\/Images\/ImageLibrary\/DAT_2456685.html\" target=\"_blank\" rel=\"noopener\">Image Library<\/a>.)<\/p>\n\n\n\n<p>Take another look at that image over the Black Sea. See how the biggest snow band extends south (and curving to the southeast) from the southern tip of the Crimean Peninsula? That is an example of how topography impacts these snow events. Due to differences in friction, surface winds are slightly more backed over land than over water, therefore areas of enhanced surface convergence exist downwind of peninsulas. The snow bands are more intense in these regions of enhanced convergence. There are also bigger than normal snow bands downwind of the easternmost and westernmost tips of Crimea, and extending south from every major point along the west coast of the Black Sea. This is not a coincidence. Land-sea (or land-lake) interactions explain this. Go back and listen to the VISIT training session for more information.<\/p>\n\n\n\n<p>Sea-effect snow affects other parts of the globe as well. It&#8217;s why the western half of Honshu (the big island of Japan) and Hokkaido are called &#8220;<a href=\"http:\/\/en.wikipedia.org\/wiki\/Snow_country_%28Japan%29\" target=\"_blank\" rel=\"noopener\">Snow Country<\/a>&#8220;. Japan was also hit with a <a href=\"http:\/\/www.presstv.ir\/Detail\/2015\/01\/08\/392138\/Northern-Japan-in-standstill-over-snowstorm\" target=\"_blank\" rel=\"noopener\">major sea-effect snowstorm<\/a> last week and, of course, VIIRS caught it:<\/p>\n\n\n\n<figure class=\"wp-block-image\"><a href=\"https:\/\/rammb2.cira.colostate.edu\/jpss-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150108_0348121_0353525.png\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"879\" src=\"https:\/\/rammb2.cira.colostate.edu\/jpss-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150108_0348121_0353525-1024x879.png\" alt=\"VIIRS &quot;Natural Color&quot; RGB composite, taken 03:48 UTC 8 January 2015\" class=\"wp-image-2444\" srcset=\"https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150108_0348121_0353525-1024x879.png 1024w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150108_0348121_0353525-300x258.png 300w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150108_0348121_0353525-768x660.png 768w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150108_0348121_0353525-1536x1319.png 1536w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150108_0348121_0353525-2048x1759.png 2048w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption class=\"wp-element-caption\">VIIRS &#8220;Natural Color&#8221; RGB composite, taken 03:48 UTC 8 January 2015.<\/figcaption><\/figure>\n\n\n\n<p>See the clear skies over Korea and the cloud streets that formed over the Sea of Japan? Classic sea-effect clouds. You can even see snow all along the west coast of Honshu in between the breaks in the clouds. Topographic impacts are once again visible. Notice the intense snow band extending southeast from the southern tip of Hokkaido\/northern tip of Honshu similar to the super-strength snow band off of Crimea. And there&#8217;s another one downwind of the straits between Kyushu and Shikoku. Another detail in this image you should have noticed is the impact that Jeju Island has on the winds and clouds. Those are classic <a href=\"http:\/\/en.wikipedia.org\/wiki\/K%C3%A1rm%C3%A1n_vortex_street\" target=\"_blank\" rel=\"noopener\">von K\u00e1rm\u00e1n vortices<\/a> which we have <a href=\"https:\/\/rammb.cira.colostate.edu\/projects\/npp\/blog\/index.php\/uncategorized\/cape-verde-waves-and-plumes\/\" target=\"_blank\" rel=\"noopener\">discussed before<\/a>.<\/p>\n\n\n\n<p>Fortunately, 8 January 2015 was near a full moon, so the Day\/Night Band was able to capture a great image of these von K\u00e1rm\u00e1n vortices:<\/p>\n\n\n\n<figure class=\"wp-block-image\"><a href=\"https:\/\/rammb2.cira.colostate.edu\/jpss-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_DNB_20150107_1809137_1814541_with_tc.png\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"837\" src=\"https:\/\/rammb2.cira.colostate.edu\/jpss-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_DNB_20150107_1809137_1814541_with_tc-1024x837.png\" alt=\"VIIRS Day\/Night Band image, taken 18:09 UTC 7 January 2015\" class=\"wp-image-2445\" srcset=\"https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_DNB_20150107_1809137_1814541_with_tc-1024x837.png 1024w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_DNB_20150107_1809137_1814541_with_tc-300x245.png 300w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_DNB_20150107_1809137_1814541_with_tc-768x628.png 768w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_DNB_20150107_1809137_1814541_with_tc-1536x1255.png 1536w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_DNB_20150107_1809137_1814541_with_tc-2048x1673.png 2048w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption class=\"wp-element-caption\">VIIRS Day\/Night Band image, taken 18:09 UTC 7 January 2015.<\/figcaption><\/figure>\n\n\n\n<p>So, to the people of the Great Lakes: Remember you&#8217;re not alone. There are people in Turkey and Japan who know what you go through every winter.<\/p>\n\n\n\n<p>&nbsp;<\/p>\n\n\n\n<p>UPDATE #1: While I was aware (and now you are aware) that sea-effect snow can impact <a href=\"http:\/\/en.wikipedia.org\/wiki\/Cape_Cod\" target=\"_blank\" rel=\"noopener\">Cape Cod<\/a>, it was brought to my attention that there is a sea-effect snow event going on there today (13 January 2015). Here&#8217;s what VIIRS saw:<\/p>\n\n\n\n<figure class=\"wp-block-image\"><a href=\"https:\/\/rammb2.cira.colostate.edu\/jpss-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150113_1729410_1732306.png\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"851\" src=\"https:\/\/rammb2.cira.colostate.edu\/jpss-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150113_1729410_1732306-1024x851.png\" alt=\"VIIRS &quot;Natural Color&quot; RGB composite, taken 17:29 UTC 13 January 2015\" class=\"wp-image-2452\" srcset=\"https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150113_1729410_1732306-1024x851.png 1024w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150113_1729410_1732306-300x249.png 300w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150113_1729410_1732306-768x638.png 768w, https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-content\/uploads\/sites\/7\/2015\/01\/VIIRS_RGB_M05_M07_M10_20150113_1729410_1732306.png 1435w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption class=\"wp-element-caption\">VIIRS &#8220;Natural Color&#8221; RGB composite, taken 17:29 UTC 13 January 2015.<\/figcaption><\/figure>\n\n\n\n<p>According to sources at the National Weather Service, some places have received 2-3 cm (~ 1 inch) of snow in a four-hour period. It&#8217;s not the same as shoveling off your roof in snow up to your neck, but it&#8217;s something!<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Take a look at this image: Is this picture from A) the Keweenaw Peninsula of Michigan in 1978? B) Orchard Park, New York in November 2014 (aka &#8220;Snowvember&#8221;)? or C) \u0130nebolu, Turkey from just last week? If you pay attention to details, you will have noticed that I credited \u0130skender \u015eeng\u00f6r with the picture and [&hellip;]<\/p>\n","protected":false},"author":16,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[20,25,39,50,76,86,89,96,104,105,106,108,116,117,124,132,156,190,192,198],"class_list":["post-2419","post","type-post","status-publish","format-standard","hentry","category-uncategorized","tag-black-sea","tag-canada","tag-daynight-band","tag-false-color","tag-ice-and-snow","tag-japan","tag-korea","tag-m-10","tag-m-3","tag-m-4","tag-m-5","tag-m-7","tag-michigan","tag-middle-east","tag-natural-color","tag-new-york","tag-rgb-composite","tag-true-color","tag-turkey","tag-vortex-street"],"_links":{"self":[{"href":"https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-json\/wp\/v2\/posts\/2419","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-json\/wp\/v2\/users\/16"}],"replies":[{"embeddable":true,"href":"https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-json\/wp\/v2\/comments?post=2419"}],"version-history":[{"count":10,"href":"https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-json\/wp\/v2\/posts\/2419\/revisions"}],"predecessor-version":[{"id":4437,"href":"https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-json\/wp\/v2\/posts\/2419\/revisions\/4437"}],"wp:attachment":[{"href":"https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-json\/wp\/v2\/media?parent=2419"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-json\/wp\/v2\/categories?post=2419"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/rammb2.cira.colostate.edu\/npp-blog\/wp-json\/wp\/v2\/tags?post=2419"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}