From: on behalf of Panel Registry Subject: FW: TNG registration of ...
From: on behalf of Panel Registry Subject: FW: TNG registration of ...
From: on behalf of Panel Registry Subject: FW: TNG registration of ...
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stati<strong>on</strong> closest to the Study Area with l<strong>on</strong>ger‐term historical climate data. While this stati<strong>on</strong><br />
al<strong>on</strong>e cannot adequately represent the diversity <strong>of</strong> the varied climate c<strong>on</strong>diti<strong>on</strong>s found<br />
within the Study Area, it does provide a reference point to examine the mean and variability<br />
<strong>of</strong><br />
seas<strong>on</strong>al climate during the baseline period. This is important as both the mean and<br />
variability <strong>of</strong> seas<strong>on</strong>al temperatures affect many ecological and hydrological processes.<br />
Table 2 shows that the mean annual and maximum winter temperatures are less than 0°C<br />
for Tatlayoko Lake. The figures also reveal that the variability (standard deviati<strong>on</strong>) <strong>of</strong><br />
minimum, maximum and mean temperatures is much higher in winter than in summer.<br />
Finally,<br />
the table highlights that minimum temperatures in winter are more variable than<br />
maximum<br />
temperatures while the opposite is true in summer.<br />
Table 2: 19611990 Baseline temperature data for Tatlayoko Lake Weather Stati<strong>on</strong><br />
Tatlayoko<br />
Lake<br />
1088010<br />
Min<br />
Temp<br />
( o C)<br />
Annual Winter Summ er<br />
Mean<br />
Temp<br />
( o C)<br />
Max<br />
Temp<br />
( o C)<br />
Min<br />
Temp<br />
( o C)<br />
Mean<br />
Temp<br />
( o C)<br />
Max<br />
Temp<br />
( o C)<br />
Min<br />
Temp<br />
( o C)<br />
Mean<br />
Temp<br />
( o C)<br />
Max<br />
Temp<br />
Mean ‐3.0 3.9 10.8 ‐11.1 ‐5.8 ‐0.4 0.6 0.8 1.4<br />
St<br />
dev<br />
Source: PCIC 2008<br />
Note – The stati<strong>on</strong> elevati<strong>on</strong> is 870m<br />
( o C)<br />
0.7 0.6 0.7 1.9 1.7 1.5 7.9 14.6 21.2<br />
While temperature is a vital climate determinant, so is precipitati<strong>on</strong>. In additi<strong>on</strong> to the total<br />
precipitati<strong>on</strong>, the proporti<strong>on</strong> that falls as snow, the timing <strong>of</strong> snow melt and the variati<strong>on</strong> in<br />
snow depth between years all have important ecological and hydrological implicati<strong>on</strong>s and<br />
are likely to be affected by climate change. During the 1961‐1990 baseline period, the<br />
proporti<strong>on</strong> <strong>of</strong> total precipitati<strong>on</strong> from snowfall was 27% at Tatlayoko Lake. As indicated by<br />
the coefficients <strong>of</strong> variati<strong>on</strong> (Cf var), snowfall varies more from year to year relative to the<br />
mean than annual precipitati<strong>on</strong>. Overall, precipitati<strong>on</strong> is relatively low compared to other<br />
areas in BC.<br />
Table 3: 19611990 baseline precipitati<strong>on</strong> and snow depth for Tatlayoko Lake<br />
Weather Stati<strong>on</strong><br />
Tatlayoko<br />
Lake<br />
Precipitati<strong>on</strong><br />
(mm)<br />
Annual<br />
Rainfall (mm) Snowfall (mm)<br />
Mean 438.9 317.0 121.9<br />
St Dev 97.6 99.3 49.1<br />
Cf var 0.2 0.3 0.4<br />
Source: PCIC 2008<br />
Note: St. Dev = standard deviati<strong>on</strong>; Cf Var = coefficient <strong>of</strong> variati<strong>on</strong><br />
16