Winter/Spring Flood Potential Outlook For Northern And Eastern Maine - 02/16/2023
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WINTER/SPRING FLOOD POTENTIAL OUTLOOK
NATIONAL WEATHER SERVICE CARIBOU ME
1039 AM EST Thu Feb 16 2023
...SPRING FLOOD POTENTIAL OUTLOOK FOR NORTHERN, CENTRAL AND
DOWNEAST MAINE...
This is the fourth Winter/Spring Flood Potential Outlook for
2023, issued by the National Weather Service in Caribou, Maine.
This outlook is for Northern, Central, and Downeast Maine for the
two- week period of February 16th to March 2nd, 2023.
The potential for ice jam flooding is normal across Northern &
Central basins. The potential for ice jam flooding is below normal
across Southern basins. The potential for open water flooding at
all basins over the next two weeks is below normal.
...CLIMATOLOGICAL GUIDANCE...
Apart from a short-lived...intense Arctic outbreak in early
February the overall pattern of warmer than normal temperatures
from January has continued. Looking back on January 2023 it was
much warmer than average compared to the 1991-2020 climate
normals. It featured long stretches of above to well above average
temperatures and only brief periods of below average
temperatures. This was a result of the monthly average of the
North Atlantic Oscillation (NAO) pattern monthly mean of +1.25
standard deviation, while the Pacific North American (PNA) pattern
at +0.21 standard deviation. This typically results in higher
500mb heights over the Northeastern United States and typically a
progressive jet stream flow from west to east with brief deeper
troughing over the east. We saw anomalous higher heights for the
month over the area with nearly no blocking in the North Atlantic
resulting in generally high pressure over the North-Central
Atlantic west of Spain.
Temperatures across the area ranged from 6.5 to 9.5 degrees above
the 1991-2020 climate normals. The month only had 6 days below
average temperatures at Caribou and only 4 days below average
temperatures at Bangor. It ranked as the 4th warmest January on
record at Caribou, and the 2nd warmest at Houlton, Millinocket and
Bangor. Bangor only had one night the entire month with a low
temperature below zero and the lowest low temperature for the
month was 2 below zero. On average, Bangor observes 8 nights with
a low temperature below zero in January. At Caribou, there were
only 4 nights with a low below zero; and typically there is an
average of 15 nights with sub-zero lows. For February,
temperatures are running overall around to slightly above normal
across the Crown with most other locations 1.5 to 2.5 degrees
above normal.
Precipitation for the month ranged from 150 to 200 percent of
average across Eastern and Northern Maine. A total of 5.33 inches
of rain and melted snow & sleet was observed at Caribou which was
the 3rd highest total on record for the month of January. A total
of 5.82 inches of rain and melted snow & sleet was observed at
Bangor which is the 4th highest total on record. Liquid
precipitation (Rain, Melted Snow, Sleet and Freezing Rain) is
running above normal across the entire area for the month of
February.
The NAO Index has been positive for virtually all of January and
early February. With a positive NAO...there tends to be a very
fast zonal flow across the northern United States and southern
Canada. Any cold air in Canada is quickly shunted east into the
North Atlantic Ocean in the fast zonal flow. So...Arctic
intrusions...although not impossible...tend to be short lived and
quickly moderate. This is exactly the scenario we saw earlier this
month. Very cold temperatures were quickly replaced with much
above normal temperatures in roughly a 48-hour period. There are
some signs that the NAO may weaken or perhaps try and turn
negative as we near the end of February or early March. If this
happens...temperatures would likely turn much more seasonal and
there would be a better chance to see increased snowfall.
The PNA pattern has been neutral to slightly positive so far this
February. There are signs that the PNA index will be turning a
bit more negative as we head into the end of February. With a
negative PNA...upper level ridging is favored across the southeast
United States which typically results in more of a broad
southwest flow across the east coast and warmer than normal
temperatures in at least southern portions of the CWA. The
combination of a positive NAO and negative PNA is typically not
very conducive to snow across much of the area. However, medium
range numerical weather forecast models suggest the cold air may
become just entrenched enough for mainly wintry precipitation
during the last week or so of February especially across northern
Maine.
The official Climate Prediction Center (CPC) medium range
forecasts seem to agree with this scenario. Temperatures are
expected to average above normal from 20 to 24 February 2023
across all of New England. However, that trend flips during the
last week or so of February when temperatures are likely to
average below normal for all areas. Precipitation is expected to
be above normal region wide from now through the end of February.
...OBSERVED SNOW DEPTH AND WATER EQUIVALENTS...
The Maine Cooperative Snow Survey fourth survey was this week
showing a rather impressive snowpack across Northern Maine with a
below normal pack in southern areas of our forecast area. Coastal
areas from Bangor to Bar Harbor to Calais were generally reporting
5 to 10 inch snow depths with several areas at the shoreline at a
trace. Snow depths were zero to a trace at Machias. Snow water
equivalents mostly vary from 0.00 to 3.00 inches in this region.
Snow depths quickly increase nearing the Central Highlands to
Moosehead Region including Interior Downeast with 12 to 18 inches
and snow water equivalents range from 3.00 to 5.00 inches with
increased water loading of the snowpack in this region. Heading
across northern Maine, snow depths generally range from 20 to 30
inches with some higher depths up to 35 to 40 inches northwest of
Caribou into the Saint John Valley. Higher terrain areas were
observing 2 to 4 foot snow depths. Chimney Pond at Katahdin
recently reported a 48 inch snow depth...an increase of 1 inch
since the last outlook. Snow water equivalents generally range
4.00 to 8.00 inches locally higher across the peaks. The highest
snow water equivalents were found along the Big Black River at
Clayton Lake...Allagash River...Fish River and Saint John River at
Fort Kent...Aroostook River at Washburn.
...SOIL MOISTURE AND WATER SUPPLY CONDITIONS...
Frozen grounds generally 2-8 inches across the area with deeper
frost in southern areas due to less snowpack. Frozen grounds
combined with no melt has allowed for virtually no changes in soil
moisture conditions. Near surface soil moisture anomalies show
all of Eastern & Northern Maine having above to well above normal
soil moisture. The latest Palmer Drought Severity Index Map from
February 9, 2023 shows the Downeast Abnormally Wet, Greater Bangor
is Extremely Wet and much of the remaining areas are Severely to
Extremely Wet. There is below normal to well below normal soil
moisture across the far North Woods along the Quebec border. The
Palmer Index looks at conditions over the span of weeks to months.
Taking a look at groundwater monitoring wells across the region courtesy
of the United States Geological Survey (USGS), we see much of the
groundwater level observing sites are well above normal to
extremely high for early February. All reporting sites are Above
Normal in the >75th percentile range with most reporting Much
Above Normal (>90th percentile) and Calais reporting historic
levels, however there is only 23 years of data there.
Lastly, given the slow discharge of the rivers we are looking at
still very high river storages. We focus on the observations we
get for the Penobscot River basin. The Penobscot total storage as
of February 13, 2023 was 67.6% full which is 36.4% above the long
term average.
...RIVER AND ICE CONDITIONS...
As of February 15th nearly every river, stream and creek with
USGS gages in Eastern & Northern Maine are reporting being
impacted by ice. Overall, natural flows are running normal to
above normal across the entire area.
Along the Saint John headwaters there is a mix of hummocked ice
and thick sheet ice approximately 8-14 inches in spots.
Significant hummock ice was found between Allagash to the Saint
Francis to Fort Kent town line. There are some very small openings
in the narrow gauge area in Saint Francis. Ice thickness
estimates were generally 8 to 11 inches with locally thicker
chunks. There has been snowmobile activity on the river along with
moose using the ice to get across between each bankside. In Fort
Kent through to before Madawaska there is some opening but with
cold air a significant increase in ice is noted. Significant
hummock ice stretches from Madawaska to Van Buren and then
downstream to Hamlin. There are some very small openings in
Madawaska around the construction site of the new International
Bridge at the port of entry.
Along the Allagash river there is a mix of hummock ice and
thickening sheet ice with more significant ice from the Allagash
River gage to the confluence with the Saint John River. Ice
thicknesses here were ranging from 4 to 10 inches with locally
thicker ice but due to significant snowpack on the ice these are
just estimates based on wildlife activity and recreational uses.
The Aroostook river is frozen between Millinocket Lake to
Masardis with a few small leads, it is noted snowmobiles are
crossing and using the river ice to travel from Oxbow Road
indicating much thicker ice. However, upstream from the Oxbow Road
it was noted several open leads indicating extreme variations in
ice thickness. Ice thicknesses near Masardis were 5 to 9 Inches
and the USGS survey team noted the ice as 100 percent black ice.
The Aroostook River is filled with hummocked ice between the
confluence of the Scopan Stream through to Ashland before the
Sheridan Road R/R trestle. Between Wade and Presque Isle through
Washburn ice thicknesses are estimated 7 to 12 inches based solely
on wildlife activity and USGS survey team measurements. Hummocked
chunks 1-3 ft thick along banking`s and caught on islands after
water levels dropped. Presque Isle to Caribou dam features sheet
ice and large hummocked ice along the banking`s. The Caribou Dam
induced opening from the Dam shortly to the Fort Fairfield Road
bridge. Beyond the bridge downstream past the Little Madawaska
River confluence into Fort Fairfield to the New Brunswick border
the ice is very hummocked with some massive thicknesses. In the
main channel the river ice is thickening to 5-9 inches noted by
wildlife activity and occasional snowmobiles venturing out on the
ice along with human activity.
Along the Piscataquis River there are frozen sections along the
headwaters and downstream to the confluence with the Penobscot
River. Ice thickness is all over the place given the reservoir and
dam activities. However, ice thickness is thick enough to host
outdoor activities in some locations along the ice. The eastern
branch of the Penobscot River along with the North & West branches
all show several areas of hummock and thickening sheet ice. There
is significant frazil ice along with bank ice reported / noted
via USGS webcam in Bangor impacting the Penobscot and Kenduskeag.
The confluence of the Kenduskeag is mainly hummocked ice but some
sheet ice. The main channel of the Penobscot is mainly open water
with frazil in the flow. Downeast Rivers and streams have
significant ice development in this recent cold air including the
St. Croix between the dams where ice can form.
...IN CONCLUSION...
The potential for flooding due to ice jams is normal across
Northern Maine with above average flows currently occurring and
significant hummock ice there is a risk for flooding this spring
if ice jams develop. Given the above normal temperatures the ice
jam potential is now normal across the Central Highlands into
Downeast Maine. The open water flood potential is below normal
across the entire area.
The next Winter/Spring Flood Outlook will be issued on Thursday,
March 2nd.
$$
Sinko
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