Ecoblitz Weather & Flowering Phenology
Alec Brooks, Seth Miller, Eriko Sakamura
April 16, 2025
Precipitation Analysis
Stats
ANOVA Fall (RAIN_INCHES ~ factor(YEAR))
| factor(YEAR) |
2 |
0.2255026 |
0.1127513 |
5.503249 |
0.0047644 |
| Residuals |
186 |
3.8107937 |
0.0204881 |
NA |
NA |
TukeyHSD Fall (RAIN_INCHES ~ factor(YEAR))
| 2022-2021 |
-0.0142857 |
-0.0745405 |
0.0459691 |
0.8413774 |
| 2023-2021 |
0.0650794 |
0.0048246 |
0.1253341 |
0.0308070 |
| 2023-2022 |
0.0793651 |
0.0191103 |
0.1396199 |
0.0060689 |
ANOVA Spring (RAIN_INCHES ~ factor(YEAR))
| factor(YEAR) |
2 |
138.9410 |
69.470484 |
48.7219 |
0 |
| Residuals |
183 |
260.9319 |
1.425858 |
NA |
NA |
TukeyHSD Spring (RAIN_INCHES ~ factor(YEAR))
| 2022-2021 |
0.0983871 |
-0.408382 |
0.6051562 |
0.8905596 |
| 2023-2021 |
1.8806452 |
1.373876 |
2.3874143 |
0.0000000 |
| 2023-2022 |
1.7822581 |
1.275489 |
2.2890272 |
0.0000000 |
Plots



Conclusion
I dun know.
Winter Snow Analysis
Stats
Correlation Matrix SNOW_WC ~ TEMP_AVERAGE
| 2021 |
-0.4873247 |
0.3311611 |
-0.6954612 |
| 2022 |
NA |
0.0572723 |
0.0249896 |
| 2023 |
0.1379338 |
-0.3367648 |
-0.1822224 |
ANOVA Fall (SNOW_WC ~ factor(YEAR))
| factor(YEAR) |
2 |
1.061058 |
0.5305291 |
49.33138 |
0 |
| Residuals |
186 |
2.000317 |
0.0107544 |
NA |
NA |
TukeyHSD Fall (SNOW_WC ~ factor(YEAR))
| 2022-2021 |
-0.0095238 |
-0.0531787 |
0.0341311 |
0.8639202 |
| 2023-2021 |
0.1539683 |
0.1103133 |
0.1976232 |
0.0000000 |
| 2023-2022 |
0.1634921 |
0.1198371 |
0.2071470 |
0.0000000 |
ANOVA Winter (SNOW_WC ~ factor(YEAR))
| factor(YEAR) |
2 |
9359.261 |
4679.63025 |
222.0825 |
0 |
| Residuals |
234 |
4930.752 |
21.07159 |
NA |
NA |
TukeyHSD Winter (SNOW_WC ~ factor(YEAR))
| 2022-2021 |
6.598734 |
4.875964 |
8.321505 |
0 |
| 2023-2021 |
15.343038 |
13.620267 |
17.065809 |
0 |
| 2023-2022 |
8.744304 |
7.021533 |
10.467074 |
0 |
ANOVA Spring (SNOW_WC ~ factor(YEAR))
| factor(YEAR) |
2 |
39489.240 |
19744.620 |
1124.153 |
0 |
| Residuals |
183 |
3214.211 |
17.564 |
NA |
NA |
TukeyHSD Spring (SNOW_WC ~ factor(YEAR))
| 2022-2021 |
5.272581 |
3.493958 |
7.051203 |
0 |
| 2023-2021 |
33.206452 |
31.427829 |
34.985074 |
0 |
| 2023-2022 |
27.933871 |
26.155249 |
29.712493 |
0 |
Plots



Conclusion
The results of our ANOVA and Tukey HSD tests indicate that snow water
content (SNOW_WC) was significantly different across the years 2021,
2022, and 2023, with 2023 showing a much higher snowfall than the
previous two years. The extremely small p-values (p < 2e-16) suggest
that these differences are not random chance but rather a real and
substantial change in snowfall patterns. The statistical significance of
YEAR used as a predictor variable indicates that winter snowpack and
temperatures play a critical role in shaping ecological conditions for
the following spring bloom season, particularly through nighttime low
temperatures that regulate seed germination and soil moisture from slow
snowmelt. Given that spring bloomers are more sensitive to these
factors, the sharp increase in snowpack and the colder temperatures in
2023 likely created conditions that influenced which species germinated
and overall blooming cycles. In contrast, fall bloomers are better
adapted to extreme conditions, including drought and high temperatures,
meaning their germination remains more stable over multiple years
despite fluctuations in winter precipitation and temperatures. These
findings reinforce that winter conditions primarily influence spring
bloom dynamics, while fall species tend to exhibit greater resilience to
annual weather variation.
Temperature Analysis
Seasonal
Stats
ANOVA Spring TEMP_AVERAGE ~ factor(YEAR))
| factor(YEAR) |
2 |
444.0833 |
222.04167 |
3.578801 |
0.0298794 |
| Residuals |
183 |
11353.9758 |
62.04358 |
NA |
NA |
Tukey Spring (TEMP_AVERAGE ~ factor(YEAR))
| 2022-2021 |
0.1774194 |
-3.165458 |
3.5202971 |
0.9913670 |
| 2023-2021 |
-3.1854839 |
-6.528362 |
0.1573939 |
0.0654317 |
| 2023-2022 |
-3.3629032 |
-6.705781 |
-0.0200254 |
0.0482772 |
P = 0.0299, p < 0.05 significant 2023 is
different
ANOVA Spring TEMP_MAX ~ factor(YEAR)
| factor(YEAR) |
2 |
1035.624 |
517.8118 |
4.670196 |
0.0105154 |
| Residuals |
183 |
20290.274 |
110.8758 |
NA |
NA |
Tukey Spring (TEMP_MAX ~ factor(YEAR))
| 2022-2021 |
-0.6290323 |
-5.097828 |
3.8397632 |
0.9408623 |
| 2023-2021 |
-5.2903226 |
-9.759118 |
-0.8215271 |
0.0156669 |
| 2023-2022 |
-4.6612903 |
-9.130086 |
-0.1924949 |
0.0386952 |
P = 0.0105, significant 2023 is different
ANOVA Spring TEMP_MIN ~ factor(YEAR)
| factor(YEAR) |
2 |
132.2258 |
66.11290 |
1.444864 |
0.238455 |
| Residuals |
183 |
8373.5645 |
45.75718 |
NA |
NA |
Tukey Spring (TEMP_MIN ~ factor(YEAR))
| 2022-2021 |
0.983871 |
-1.886921 |
3.8546628 |
0.6974276 |
| 2023-2021 |
-1.080645 |
-3.951437 |
1.7901467 |
0.6476309 |
| 2023-2022 |
-2.064516 |
-4.935308 |
0.8062757 |
0.2082135 |
P = 0.238, NOT significant All same/similar
ANOVA Fall TEMP_AVERAGE ~ factor(YEAR)
| factor(YEAR) |
2 |
734.0511 |
367.02554 |
5.645152 |
0.0041783 |
| Residuals |
183 |
11897.9395 |
65.01606 |
NA |
NA |
Fall (TEMP_AVERAGE ~ factor(YEAR))
| 2022-2021 |
4.1774194 |
0.7554005 |
7.5994382 |
0.0121575 |
| 2023-2021 |
-0.0725806 |
-3.4945995 |
3.3494382 |
0.9986162 |
| 2023-2022 |
-4.2500000 |
-7.6720188 |
-0.8279812 |
0.0104769 |
P < 0.05, P = 0.00418, significant, 2022 is
different
ANOVA Fall TEMP_MAX ~ factor(YEAR)
| factor(YEAR) |
2 |
1191.946 |
595.9731 |
5.94926 |
0.003139 |
| Residuals |
183 |
18332.210 |
100.1760 |
NA |
NA |
Tukey Fall (TEMP_MAX ~ factor(YEAR))
| 2022-2021 |
3.790323 |
-0.4573783 |
8.038023 |
0.0908995 |
| 2023-2021 |
-2.354839 |
-6.6025396 |
1.892862 |
0.3914470 |
| 2023-2022 |
-6.145161 |
-10.3928622 |
-1.897460 |
0.0022303 |
P = 0.00314 significant 2022 is different
ANOVA Fall TEMP_MIN ~ factor(YEAR)
| factor(YEAR) |
2 |
646.0968 |
323.0484 |
5.960566 |
0.0031059 |
| Residuals |
183 |
9918.1613 |
54.1976 |
NA |
NA |
Tukey Fall (TEMP_MIN ~ factor(YEAR))
| 2022-2021 |
4.564516 |
1.440149 |
7.6888836 |
0.0019882 |
| 2023-2021 |
2.209677 |
-0.914690 |
5.3340448 |
0.2190695 |
| 2023-2022 |
-2.354839 |
-5.479206 |
0.7695287 |
0.1788433 |
P = 0.00311 significant, 2022-2021 is
different??
Mean Temperatures for Spring and Fall (2021-2023)
| 2021 |
51.10484 |
68.74194 |
| 2022 |
51.28226 |
72.91935 |
| 2023 |
47.91935 |
68.66935 |
Plots



Week 1 Temperature Analysis
Stats
ANOVA Spring week 1 - TEMP_AVERAGE ~ factor(YEAR)
| factor(YEAR) |
2 |
618.4524 |
309.2262 |
7.273873 |
0.0048391 |
| Residuals |
18 |
765.2143 |
42.5119 |
NA |
NA |
Tukey Spring week 1 - ANOVA(TEMP_AVERAGE ~
factor(YEAR))
| 2022-2021 |
-7.857143 |
-16.75181 |
1.037524 |
0.0888148 |
| 2023-2021 |
-13.214286 |
-22.10895 |
-4.319619 |
0.0036348 |
| 2023-2022 |
-5.357143 |
-14.25181 |
3.537524 |
0.2978214 |
P = 0.000484, P < 0.05 significant, 2021 is different with
90% sig level
ANOVA Spring week 1 - TEMP_MAX ~ factor(YEAR)
| factor(YEAR) |
2 |
1245.81 |
622.90476 |
8.787058 |
0.0021739 |
| Residuals |
18 |
1276.00 |
70.88889 |
NA |
NA |
Tukey Spring week 1 - ANOVA(TEMP_MAX ~ factor(YEAR))
| 2022-2021 |
-11.428571 |
-22.91443 |
0.057288 |
0.0512770 |
| 2023-2021 |
-18.714286 |
-30.20015 |
-7.228426 |
0.0016276 |
| 2023-2022 |
-7.285714 |
-18.77157 |
4.200145 |
0.2635155 |
P = 0.00217, significant, 2021 is different with 90% sig
level
ANOVA Spring week 1 - TEMP_MIN ~ factor(YEAR)
| factor(YEAR) |
2 |
209.1429 |
104.5714 |
2.904762 |
0.080667 |
| Residuals |
18 |
648.0000 |
36.0000 |
NA |
NA |
Tukey Spring week 1 - ANOVA(TEMP_MIN ~ factor(YEAR))
| 2022-2021 |
-4.285714 |
-12.47085 |
3.8994172 |
0.3941497 |
| 2023-2021 |
-7.714286 |
-15.89942 |
0.4708458 |
0.0666534 |
| 2023-2022 |
-3.428571 |
-11.61370 |
4.7565601 |
0.5446789 |
P = 0.0807, NOT significant, 2023-2021 is
different
ANOVA Fall week 1 TEMP_AVERAGE ~ factor(YEAR)
| factor(YEAR) |
2 |
487.1667 |
243.58333 |
12.04297 |
0.0004789 |
| Residuals |
18 |
364.0714 |
20.22619 |
NA |
NA |
Tukey Fall week 1 - ANOVA(TEMP_AVERAGE ~
factor(YEAR))
| 2022-2021 |
-5.428571 |
-11.56381 |
0.7066672 |
0.0881956 |
| 2023-2021 |
-11.785714 |
-17.92095 |
-5.6504757 |
0.0003220 |
| 2023-2022 |
-6.357143 |
-12.49238 |
-0.2219042 |
0.0415794 |
P < 0.05, P = 0.000479, significant, 2023 is
different
ANOVA Fall week 1 TEMP_MAX ~ factor(YEAR)
| factor(YEAR) |
2 |
1469.2381 |
734.61905 |
14.39533 |
0.0001845 |
| Residuals |
18 |
918.5714 |
51.03175 |
NA |
NA |
Tukey Fall week 1 Max - ANOVA(TEMP_MAX ~
factor(YEAR))
| 2022-2021 |
-8.857143 |
-18.60243 |
0.888144 |
0.0785563 |
| 2023-2021 |
-20.428571 |
-30.17386 |
-10.683285 |
0.0001240 |
| 2023-2022 |
-11.571429 |
-21.31672 |
-1.826142 |
0.0187604 |
P = 0.000185 significant, 2023 is different
ANOVA Fall week 1 TEMP_MIN ~ factor(YEAR)
| factor(YEAR) |
2 |
35.42857 |
17.714286 |
1.910959 |
0.1767732 |
| Residuals |
18 |
166.85714 |
9.269841 |
NA |
NA |
Tukey Fall week 1 Min - ANOVA(TEMP_MIN ~
factor(YEAR))
| 2022-2021 |
-2.000000 |
-6.153465 |
2.153465 |
0.4520604 |
| 2023-2021 |
-3.142857 |
-7.296322 |
1.010608 |
0.1587432 |
| 2023-2022 |
-1.142857 |
-5.296322 |
3.010608 |
0.7652385 |
P = 0.177 NOT significant, All same
Plots



Conclusion
Our temperature analysis reveals that Spring 2023 was significantly
colder than previous years, with average and maximum temperatures
showing a notable decline, particularly in Week 1. This suggests that
spring species were impacted by colder temperatures and (in conjunction
with the snow fall analysis) heavy snowfall, likely delaying growth. As
spring bloomers are more sensitive to winter conditions, variation in
nighttime low temperatures and soil moisture retention from slow
snowmelt could explain the shifts in bloom timing and species. However,
our analysis did not identify clear trends between temperature and total
plant volume across years, suggesting that there may be an ecological
threshold where additional moisture does not always lead to increased
plant germination and growth. In contrast, fall temperatures fluctuated,
with 2022 being significantly warmer than both 2021 and 2023, yet these
variations did not disrupt fall bloom patterns. Since fall species are
more adapted to germinating in harsh conditions—including high
temperatures and low precipitation—their bloom cycles appear more
consistent despite annual shifts in seasonal climate variables. These
findings support the idea that spring bloomers experience more
variability in response to weather patterns, whereas fall species
exhibit greater resilience to changing environmental conditions.