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| Current Grand Rapids Area
Assessment Images At A Glance |
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UPDATE
IMAGES BY PUSHING "F5" OR
"SHIFT/REFRESH" |
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Current Conditions & Zone Forecast For Grand Rapids |
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| Additional
Assessment Images |
| MORE
ASSESSMENT IMAGE DISPLAYS |
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| SEVEN-DAY
FORECAST IMAGES |
| MICHIGAN
REGION DOPPLER RADAR SITES - NWS |
| Severe
Weather & Related Information (Text-based) |
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| The Day
1 Convective Outlook, Day
2 Convective Outlook and Day
3 Convective Outlook are guidance products issued by
the SPC Operational Branch in Norman, Oklahoma. The Day 1
outlook outlines areas in the continental United States
where severe thunderstorms may develop during the next 6 to
73 hours. The Day 1 Convective Outlook is issued 5 times
daily: at 06Z (the initial day-1 outlook, valid 12Z that day
until 12Z the following day), 13Z and 1630Z (the
"morning updates," valid until 12Z the next day),
20Z (the "afternoon update," valid until 12Z the
next day), and the 01Z (the "evening update,"
valid until 12Z the following day). |
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| GRAND RAPIDS (GRR) NWS PRODUCTS |
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| NATIONAL CONVECTIVE STATEMENTS |
| MICHIGAN STATE POLICE REPORTS |
| Quick Links To GRR Zone Products |
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| CURRENT
WEATHER OBSERVATIONS - MICHIGAN AWOS/ASOS INSTALLATIONS |
| Automated Weather Observation Systems (AWOS) and Automated Surface Observation Systems (ASOS) are installed at airports across the state. They provide weather observations 24 hours a day without human involvement. The systems report wind speed and direction, ceiling, visibility, temperature, dew point, barometric pressure, and any recorded remarks. Those systems with "present weather" sensors also report cloud cover and height,
and precipitation type. State-owned AWOS systems are installed and maintained by the Bureau of Aeronautics in cooperation with each airport. For additional information and details about each Michigan AWOS/ASOS site, including frequency and telephone access, please
click
here. |
| MICHIGAN
REGIONAL SURFACE CONDITIONS & WEATHER DATA PAGE - UCAR |
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| UPPER AIR TEMPS & HUMIDITY |
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Precipitable Water
This is a contour plot of precipitable water in inches. The
contour interval is .2 inches. Precipitable water reflects the amount of water contained
in a vertical column above the surface if it were all precipitated out. This is a good
indicator of how much rain or snow might fall as a result of a thunderstorm or low
pressure system. To roughly figure your possible rainfall, find how much precipitable
water you have overhead, multiply by your humidity (i.e. x .74), divide by 24 to get how
much per hour, estimate how much actual time it will precipitate by looking at radar, then
multiply by how many hours to get the total amount. |
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Precipitable Water Composite - UNISYS |
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Precipitable Water - OSU |
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WINDS/TEMPS
ALOFT (Constant Pressure Plots)
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850 mb
or about
5,000'
MSL |
700 mb
or about
10,000
MSL |
500 mb
or about
18,000"
MSL |
300 mb
or about
30,000'
MSL |
250 mb
or about
35,000'
MSL |
200 mb
or about
38,500'
MSL |
| NCAR |
NCAR |
NCAR |
NCAR |
NCAR |
NCAR |
| OSU |
OSU |
OSU |
OSU |
OSU |
OSU |
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DISPLAY ALL
UPPER AIR
INDICES IMAGES |
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Lifted Index
This is an index used to determine the stability of the lower
half of the troposphere. The LI field shows instability in the atmosphere by lifting a
parcel of air from the surface to 500 mb and comparing its temperature to that of the
environment. Where LIs are less than 0, thunderstorms are possible. The lower the number,
the more unstable the atmosphere is and as a result, the stronger the thunderstorms could
become. Values of -4 or lower indicate areas where severe thunderstorms are possible.
Values > 10 indicate areas of stable weather where skies are generally clear. The risk
of severe weather activity is defined as follows:
LI > 2 No significant activity
0 < LI < 2 Showers probable, isolated thunderstorms possible
-2 < LI < 0 Thunderstorms probable
-4 < LI < -2 Severe thunderstorms possible
LI < -4 Severe thunderstorms probable, tornadoes possible
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Lifted Index - OSU |
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Surface To 500 mb Lifted Index
- UNISYS |
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Theta-E
Another instability tool. Ridges indicate unstable air. |
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Theta-E Plot - UCAR |
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K-Index
The K Index field shows instability in the atmosphere as it
relates to the development of air mass thunderstorms. The KI is similar to Total Totals
index except that it takes into account moist air at 700 mb contributing to air mass
thunderstorm development. It is based on the 850 to 500 mb lapse rate plus 850 mb dewpoint
minus the 700 mb dewpoint depression. It is defined as follows: K = T850 - T500 + Td850 -
(T700 - Td700). Strong Springtime thunderstorms often require dry air at mid levels to cap
the convection. On the other hand, summer air mass thunderstorms need a very moist
atmosphere at mid levels to prevent evaporation through entrainment. Where KIs are greater
than 35, air mass thunderstorms are likely. the higher the number, the higher the
probability. Values < 10 indicate areas of stable weather where skies are generally
clear. The risk of air mass thunderstorms is defined as follows:
K < 15 0% Air mass t-storm probability
15-20 <20% Air mass t-storm probability
21-25 20-40% Air mass t-storm prob.
26-30 40-60% Air mass t-storm prob.
31-35 60-80% Air mass t-storm prob.
36-40 80-90% Air mass t-storm prob.
K > 40 >90% Air mass t-storm probability
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K-Index - UNISYS |
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K-Index - OSU |
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Showalter Index
This is an index used to determine the stability of the lower
half of the troposphere. An air parcel is lifted from an initial position at 850 mb where
localized low level influences are greatly reduced. It is lifted dry adiabatically to its
LCL and then pseudo-adiabatically to 500 mb. The environmental temperature is then
subtracted from the parcel temperature to obtain the value of the Showalter index. The
risk of severe weather activity is defined as follows:
SI > 3 No significant activity
1 < SI < 3 Showers probable, isolated thunderstorms possible
-2 < SI < 1 Showers probable, isolated thunderstorms possible
-2 < SI < 1 Thunderstorms probable
-6 < SI < -2 Severe t-storms possible
SI < -6 Tornadoes possible
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Showalter Index - OSU |
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Vertical Total Totals Index
A measure of the thunderstorm potential, according to the
following scale and color fill scheme:
< 25 Thunderstorms unlikely
25-26 Scattered thunderstorms
27-30 Scattered t-storms/ few severe/ isolated tornadoes
31-32 Scattered-numerous t-storms/ few tornadoes
33-34 Numerous thunderstorms/ few tornadoes
> 34 Numerous t-storms/ scattered severe/scattered tornadoes
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Vertical Total Totals Plot - OSU |
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| Providing satellite, radar and data analyses, as well as model forecasts
from the National Centers for Environmental Prediction (NCEP) operational
ETA, NGM or Aviation (AVN) models.
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GOES SOUNDINGS PRODUCTS
DATA - NOAA/NESDIS
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| Horizontal
Soundings Fields |
TPW, LI, CAPE, and CINH fields. Full U.S., Pacific, and Regional
displays |
| Archive
of Soundings Fields |
24 hour archive of TPW, LI, CAPE, 850mb Temp, 700mb Temp, and 500mb
Temp fields (for various regions) |
| Vertical
Sounding Profiles |
Hourly Skew-T diagrams for over 450 sites across the U.S., Mexico,
Caribbean, W Atlantic, E Pacific, and S Canada (including 24hr
archive) |
| Vertical
Profile Loops |
24 hour JAVA loops of Skew-T diagrams for all above mentioned 450
sites |
| Cross
Sections |
Theta-E, Mixing Ratio, RH, and Wet Bulb cross sections for 18 selected
pairs of end points |
| Cross
Section Loops |
Theta-E, Mixing Ratio, RH, and Wet Bulb cross section loops for 18
selected pairs of end points |
| 3-Hour
Time Difference Fields |
TPW, LI, CAPE, and CINH fields showing 3 hour changes for various U.S.
regional sectors |
| Colorized
Soundings Imagery |
Colorized maps of various derived Soundings parameters over
concatenated GOES-East and GOES-West sectors |
| Colorized
Soundings Loops |
Colorized loops of various derived Soundings parameters over
concatenated GOES-East and GOES-West sectors |
| PW
Coverage and Adjustments |
Display showing latest GOES Soundings coverage with color coding
showing GOES adjustments to first guess |
| Raw
Soundings Files |
Binary format and McIDAS format Soundings data |
| Lake
Effect Snow Support |
Hourly GOES Total Precipitable Water Estimates for Great Lakes Region
(Seasonal) |
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SkewT diagrams are derived using
data collected by radiosondes, carried by balloon, and released
twice each day (00 & 12 UTC) at more than 1000 sites worldwide. This thermodynamic diagram, or SkewT/LogP diagram, also known as a sounding, is a graph showing the vertical distribution of the temperature, dew point, wind direction, and wind speed of the radiosonde as it rises through the atmosphere
(up an altitude of about 30 km or 100,000 feet) near the site where
it was launched. For more information, check out these excellent
guides to Skew-T's from OSU
& NEMAS. |
| NPN
WIND PROFILERS - UCAR |
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It is very important to severe weather forecasting to know what the upper level winds are doing - much more often than the twice daily balloon soundings. Hourly upper air winds are available through displays of radar-derived winds. The winds are detected by a network of wind profilers - Doppler radars with stationary antennae, pointed straight upward - that can "see" which way the air is moving and how fast it's moving. The system is called a "profiler" because it gives air speed and direction data from near the surface to above the tropopause, thus it provides a vertical profile of the earth's atmosphere. |
| Analysis
& Forecast Models |
For
additional Great Lakes area surface and upper air analysis
graphics, visit our new RUC Analysis & Forecast
page. The FSL
RUC ANALYSIS & FORECAST MAPS
(RUC - Rapid Update Cycle)
is an operational atmospheric prediction system comprising
primarily of a numerical forecast model and an analysis system
to initialize that model. MAPS is the research counterpart to
the RUC. The RUC has been developed to serve users needing
short-range weather forecasts, including those in the US
aviation community. |
| ADDITIONAL
NUMERICAL MODEL SOURCES |
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| QUESTIONS/ COMMENTS? |
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feel free to email
WeatherMichigan.com with your
questions, comments, or suggestions. We want to
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well, but please be constructive. And if you
know of any Michigan weather-related image or
link that should be included on this site, write
us. |
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