“It Came from Nunavut”
It sounds like the title of a good movie to describe this cold weather. Have you been wondering where this system came from? The upper-level low pressure system dived down from northwest Nunavut, in far northern Canada, to Minnesota. pic.twitter.com/GZSMCcO1eR— NWS Duluth (@NWSduluth) January 30, 2019
GOES-16 “Clean” Infrared Window (10.3 µm) images (below) also showed the southward expansion of arctic air into the north-central US — surface infrared brightness temperatures of -30 to -40ºC (darker blue to green enhancement) covered a large area. Such cold infrared brightness temperatures are normally associated with clouds in the middle to upper troposphere. Surface air temperatures of -20 to -40ºF were widespread, along with wind chill values of -40 to -70ºF, leading to numerous school and business closures. Two of the coldest official temperatures in the US on the morning of 30 January were -48ºF at Norris Camp, Minnesota and -44ºF at Bottineau, North Dakota (the high temperature in Bottineau on the previous day, 29 January, was only -26ºF); however, there were a few North Dakota Department of Transportation roadside sensors that reported low temperatures of -49ºF.
More than 130 hourly observation stations across the Upper Midwest recorded a wind chill of -50°F or colder overnight into this morning. Here are some select station minimums from across the region. pic.twitter.com/A7FXAKdP8y
— MRCC (@MidwestClimate) January 30, 2019
GOES-16 True Color RGB images (below) revealed a variety of multiple-band and single-band lake effect snow features as the arctic air moved across the Great Lakes. In addition, elongated and long-lived cloud bands created snow squall conditions across parts of Ohio and Pennsylvania.
VIIRS True Color RGB and Infrared Window (11.45 µm) images from NOAA-20 (at 1802 UTC) and Suomi NPP (at 1852 UTC) viewed using RealEarth (below) provided a closer look at the cloud bands across Ohio and Pennsylvania.![True Color RGB and Infrared Window (11.45 µm) images from NOAA-20 (at 1802 UTC) and Suomi NPP (at 1852 UTC) [click to enlarge]](https://cimss.ssec.wisc.edu/goes/blog/wp-content/uploads/2019/01/190130_18utc_noaa20_suomiNPP_viirs_OH_PA_snow_squalls_anim.gif)
VIIRS True Color RGB and Infrared Window (11.45 µm) images from NOAA-20 (at 1802 UTC) and Suomi NPP (at 1852 UTC) [click to enlarge]
A toggle between Terra MODIS True Color RGB images (below) showed growth of the nearshore ice in Lake Michigan around the Chicago area.
from CIMSS Satellite Blog http://cimss.ssec.wisc.edu/goes/blog/archives/31518
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