Cape Breton Post

Climate calendar changes

November has been known as the time for rivers to freeze

- Annamarie Hatcher

It is November in the Bras d’Or Lake Biosphere and in the Mi’kmaq calendar that is “rivers starting to freeze time” (Keptekiwik­u’s).

As I think back over autumns in the past I am wondering whether the rivers will actually start to freeze in November and how that may change with our changing climate. Shall we think about re-naming Keptekiwik­u’s?

Let’s examine this proposal. The calendar on my wall, computer and cellphone is called the Gregorian calendar after Pope Gregory XIII who introduced it in 1582. It is a solar calendar based on a 365-day year divided into 12 months of irregular lengths with an extra day added nearly every four years. Many great minds came up with that plan but it took a pope to put it in place.

Although we attempt to track Mi’kmaq months as our common months based on the Gregorian calendar, they are not really equivalent. There are actually 13 moon cycles in the traditiona­l Mi’kmaq calendar every year. Each cycle starts with the new moon and is named after a significan­t environmen­tal occurrence at that time.

The Mi’kmaq calendar is a lunar calendar with 13 lunar months making up a year. A lunar month is equivalent to the time that the moon takes to pass through each of its phases (new moon, half-moon and full moon) and return back to its original position. This takes approximat­ely 29.5 days. A lunar year has approximat­ely 354 days.

The Gregorian calendar is based on a solar year which has about 365 days. This leaves an 11-day difference between one solar year and one lunar year and at least part of a 13th month. This year, the November moon is Nov. 6-Dec. 6. Does that time period seem more likely for “rivers starting to freeze?”

Ice-up conditions at two Environmen­t Canada stream gauging stations reported over the last 10-12 years may provide insight into freezing patterns in the biosphere.

Ice formation in the Middle River can start as early as Dec. 4, as was measured in 2007, and Nov. 29 in the River Denys, as noted that same year.

However, timing of ice formation depends upon the hydrology of the river (water velocities and the inflow of warmer ground water).

In Glen Brook, near Melford, temperatur­es measured during some November days showed a huge range, from 1.7 to 10 between 2001 and 2015. So, rivers may start to freeze during Keptekiwik­u’s but it is probably a bit of shell ice in the shallows and it is dependent on time, location and geology in the Bras d’Or Lake Biosphere.

The Bras d’Or Lake Biosphere is in the centre of Unama’ki, one of the seven traditiona­l districts of Mi’kma’ki. The original seven districts extend from the Gaspe region of Quebec to the northern part of Maine.

Present day conditions for “rivers starting to freeze” are clearly more probable near the northern parts of Mi’kma’ki.

For example, air temperatur­es monitored by Environmen­t Canada at the South Tetagouche station near Bathurst, N.B., yielded much lower climate-normal temperatur­es than Baddeck during November for the years 1981 to 2010. Although I don’t have water temperatur­es from that area, those air temperatur­es say to me that rivers starting to freeze is a very likely scenario during the November moon in South Tetagouche. Ice-up in the Petitcodia­c River near Moncton, in the middle of Mi’kma’ki supports that conclusion.

In a technical report by D. Caissie in 2000 (Canadian Technical Report of Fisheries and Aquatic Sciences 2301) it was shown that ice-up occurred before Nov. 11 on average 77 per cent of the time between 1962 and 1996. It seems likely that the November moon may have earned its name in one of the other districts of Mi’kma’ki.

With a changing climate and warming oceans, the time gap between the November moon and Keptekiwik­u’s, or rivers starting to freeze time, is likely to widen. Because we are surrounded by water, our climate is strongly influenced by oceanic processes.

This end of the province is influenced by the northerly flowing Labrador current whereas the southern end feels the influence of the warm Gulf Stream. So, if we look closely at the scientific modelling relating global climate change to the Labrador current, the picture is clear. We are in for a warmer ocean and warmer Novembers in the future with the gap between the November moon and “rivers starting to freeze” ever widening.”

 ?? CONTRIBUTE­D ?? Major currents of the Northeast Atlantic — warm currents are coloured with reds and colder currents with blues; the Gulf of Maine study area is shaded in yellow. The underlying image shows bathymetry with darker blues representi­ng deeper water.
CONTRIBUTE­D Major currents of the Northeast Atlantic — warm currents are coloured with reds and colder currents with blues; the Gulf of Maine study area is shaded in yellow. The underlying image shows bathymetry with darker blues representi­ng deeper water.
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