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GCPEx: GPM Cold-season Precipitation Experiment
Overview
The GPM Cold-season Precipitation Experiment (GCPEx) was conducted in cooperation with Environment Canada in Ontario, Canada from January 17th to February 29th, 2012. The overarching goal of GCPEx was to characterize the ability of multi-frequency active and passive microwave sensors to detect and estimate falling snow through the collection of microphysical property data, associated remote sensing observations, and coordinated model simulations of falling snow. Through collection of these unique datasets, GCPEx's goal is to improve the GPM snowfall retrieval algorithms.
The GCPEx experiment used instrumented aircraft (NASA DC-8, NASA-funded University of North Dakota Cessna Citation, and Canadian National Research Council Convair 580) for flights over heavily-instrumented ground sites located in and around the Environment Centre for Atmospheric Research Experiments (CARE) located in Egbert, Ontario. The DC-8 aircraft flew high above clouds and precipitation with instruments similar to those on the GPM Core satellite. The Citation and C580 aircraft also flew through snowing clouds to measure snowflake properties in situ. Ground-based equipment such as radars and surface particle and snow water equivalent measurement instrumentation connected airborne measurements of snowfall to what was measured at the ground. Data from the experiment will be used to develop and validate snow and frozen precipitation retrieval algorithms used in the generation of data products for GPM, CloudSat and future polar precipitation missions planned by the European Union.
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Learn more about GCPEx:
- Scientific Motivation and Goals
- Measuring Frozen Precipitation from Space
- Cloud Resolving Model (CRM) Simulations
- GCPEx Field Site
- Observational Strategy and Instruments
Campaign Blog
Thursday, February 16, 2012
By Chris Kidd
NASA scientist Chris Kidd shared some of his photos from the last several days at GCPEx.
Monday, February 13, 2012
By Ellen Gray
Lake effect snow forms when cold winds pick up moisture and energy as they pass over long stretches of warmer bodies of water. In this case, the cold wind passed over Lake Huron, and the water vapor from the lake collected into the clouds and froze into snow. The snow falls in bands, and with the wind strength directing where the most moisture gets picked up and then dumped, the amount of snowfall on the ground can vary quite a bit from place to place, even those as close as the CARE site and...
Wednesday, February 8, 2012
By Gail Skofronick-Jackson
Models showed quickly developing snow from 9-10pm EST tonight (6 Feb 2012). We are at 9:22 and we don't yet see snow in the real time ground radar data. The DC-8 is up and flying back and forth, waiting, waiting, waiting for the snow. We aren't sending up the Citation until we see snow on the ground radars.
Tuesday, January 31, 2012
By Joe Munchak
It’s been a relatively eventful few days here in Barrie, Ontario, with two coordinated air-ground campaigns over the past three days. I was actually driving to Barrie from my home in Maryland during the first event (Jan 28), and got to experience some lake effect snow bands first-hand in northern Pennsylvania on my way up. These were very narrow, only a few miles wide, but heavy enough to drop an inch or two during the 15 minutes or so I encountered them! Fortunately, temperatures were...
Thursday, January 26, 2012
By Ellen Gray
This image of falling snowflakes was taken by the Snow Video Imager (SVI) at one of the auxiliary ground sites, the Steamshow Fairgrounds, 5 miles (8km) south of the main CARE site, during a light snowfall on Saturday, January 21. The SVI is set up about two feet off the ground and the snowflakes are falling from top to bottom through the frame. They can be seen here in different three-dimensional orientations at 5x magnification.
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