F. Fazel-Rastgar
DOI:
10.4236/ajcc.2020.92008 104
American Journal of Climate Change
the lowest slope during spring (Figure 2). The sub anomaly period (1999-2015)
from the recent 2 decades has been selected for statistical analysis which is pre-
sented in the Section 17.
Figure 3 shows sea surface temperature (SST) anomaly map during 1998-2018
(study period) departure from 1981-2010 (normal period) for winter (a), spring
(b), summer (c) and fall (d) in Hudson Bay region. The sea surface temperatures
have been increased in Hudson Bay. During winter, the highest value is ~2.5 K
in the north and northeast. In spring the maximum change in SST is in the north
part around 1 K. During summer the areas in the west have been getting warm
with a maximum value around 1.1 K. During fall, the SST has been increased in
the west, east and north with the maximum around 1.9 K.
3.1.1. Air Temperature Anomaly at 2 m
Figure 4(a) shows 2 m air temperature anomaly in Hudson Bay region for the
study period. This figure shows the increase of 2 m air temperature in all parts of
Hudson Bay. The temperature anomaly increases from the west (around 1 K) to
the north-west, east and south-east. The increase in 2 m air temperature in the
boundary region in the north, east and south boundaries is remarkable with the
maximum value at around 4 K.
Figure 4(b) shows 2 m air temperature anomaly
during spring. The temperature at 2 m has been increased mostly in all part from
~0.2 K to ~1.8 K except the south-west part with no change.
Figure 4(c) shows
the same map but for summer anomaly. During summer, Hudson Bay (except in
(a) (b)
(c) (d)
Figure 2. Seasonal mean time series of SST for winter (a); spring (b); summer (c) and fall (d) for Hudson Bay from 1948 to 2018.
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