LakeErieWX: Understanding Meteorological Time

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Introduction

Weather recognizes no geographic or political borders. In order to coordinate their observations and forecasts, meteorologists around the world use a standard timekeeping system. The original standard timekeeping system was Greenwich Mean Time (GMT) a 24-hour clock system based on the local time in Greenwich, England. For example, 1:00 am in Greenwich is 0100 GMT, noon is 1200 GMT, and 6:00 pm is 18 GMT.

Since GMT is technically a time zone, it was replaced with Coordinated Universal Time (UTC) in the early 1970s. Similar to GMT, UTC is a 24-clock system that doesn’t recognize local adjustments such as Daylight Saving Time. The National Weather Service’s version of UTC is called Zulu, which is typically abbreviated as “Z” on their forecast maps and text products.

In order to use forecast products based on Zulu, you’ll need to convert from Zulu to your local time. Fortunately, converting is easy once you know the time difference (time zone offset) between your location and Greenwich, England. If you live in the Eastern Time zone, subtract four hours from Zulu to arrive at your local time. Residents in the Central Time zone must subtract five hours. For example, 1200Z is 8:00 am Eastern and 7:00 am Central Time. When Daylight Saving Time is not in effect, an additional hour must be subtracted — 1200Z is 7:00 am Eastern. Table 1, below, shows Zulu-to-local-time conversions for the Eastern, Central, and Pacific Time zones (click here for a larger version).

Click to enlarge.

Click to enlarge.

Interpreting Images and Converting Time

The National Weather Service and other forecast providers display Zulu time in a variety of ways. Let’s look at a few examples.

Surface Weather Forecasts: The sample surface weather forecast below (Figure 1) was issued, or published, at 1852Z on Friday, June 10, 2016. Surface weather forecasts are issued by the Weather Prediction Center and display the future position and nature of weather features such as barometric pressure, frontal boundaries, and precipitation at a specific time in the future. This future date and time of a forecast is known as its valid time. The forecast shown in Figure 1 is valid at 1200Z on Saturday, June 11, 2016. Valid is frequently abbreviated as “V.”

Figure 1: Surface weather forecast from the Weather Prediction Center.

Figure 1: Surface weather forecast from the Weather Prediction Center.

Satellite Imagery: Satellite imagery, particularly visible and infrared, can help a weather-savvy boater assess cloud coverage or the extent of severe weather. Most websites update satellite images every 30 to 60 minutes. Since conditions can change dramatically between updates, it is prudent to determine the age of the image by comparing the image’s time stamp to the current time. The sample visible image (Figure 2) was published at 2130 UTC (same as Zulu) on June 11, 2016.

Figure 2: Visible satellite image.

Figure 2: Visible satellite image.

Thunderstorm Outlooks: Thunderstorm Outlooks from the Storm Prediction Center (SPC) show the probability that thunderstorms will occur during a particular four-hour period. The sample Outlook (Figure 3) was issued at 1633Z on June 6, 2016 and was valid from 2000Z on June 7 to 0000Z on June 8.

Figure 3: Storm Prediction Center Thunderstorm Outlook.

Figure 3: Storm Prediction Center Thunderstorm Outlook.

High Resolution Wind Forecast: Penn State University (PSU) produces a wide variety of cutting-edge products that are useful to the recreational boater. However, the imagery presumes the user has a working knowledge of meteorological shorthand and timekeeping systems. The sample high-resolution wind forecast (Figure 5 is available in 1-hour increments, and its legend contains a lot of information (Figure 4)).

Figure 5: Legend for the high resolution wind forecast.

Figure 4: Legend for the high resolution wind forecast.

The first half of the first line “4km NAM 10-m Wind (KTS)” indicates the image was produced by the NAM forecast model, and has a horizontal resolution of 4 kilometers (smaller resolution is better). The image is a forecast for winds at a height of 10 meters (this is standard) and the units are in knots. The second half of the line “SAT 160611/0200V002” indicates the forecast was valid at 0200Z on Saturday, June 11, 2016. The “V002” indicates the forecast was valid 2 hours after it was initialized. The second line indicates the forecast was initialized, or processed, at 0000Z on June 11, 2016.

Figure 5: High-resolution wind forecast from Penn State University.

Figure 5: High-resolution wind forecast from Penn State University.

Conclusion

Translating legends on forecast graphics can be challenging, but the important step of converting from GMT/Zulu/UTC to your local time becomes straightforward with a little practice.

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ABOUT THE AUTHOR:

Mark began sailing on Lake Erie in 1994 and he and his wife Susan currently own Osprey, a 1985 C&C 35. His interest in weather forecasting grew from his experiences cruising and racing on the lake. In addition to sailing and forecasting, Mark enjoys publishing summaries of interesting weather events and teaching Great Lakes sailors basic weather forecasting skills.

MAThornton

Mark is a 2006 graduate of the Penn State University Certificate of Achievement in Weather Forecasting, a two-year program that develops skills in general, tropical and severe weather forecasting. He maintains a website (www.lakeeriewx.com) devoted to marine weather education and forecasting resources and is the past president of the local chapter of the American Meteorological Society. Mark is employed as the Vice-President of Administration for the law firm of Wegman, Hessler & Vanderburg and as a Teaching Assistant in the Certificate of Achievement in Weather Forecasting Program at Penn State University.

Click here to view his meteorological resume or here to read about his marine weather forecasting seminars and workshops.

This post originally appeared on Mark's LakeErieWX blog and can be found here.

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