Waiting on a mule deer crossing…
Examines how shifting snowmelt dates and frost events disrupt the flowering timing of alpine plants, particularly larkspurs, and the cascading consequences for plant-pollinator synchrony under climate change.
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In the high meadows around Gothic, Colorado, the rhythm of life is set by snow. Wildflowers bloom, bees emerge, hummingbirds arrive, and marmots wake from hibernation according to when the previous winter's snowpack finally melts away. Phenology, the study of the seasonal timing of biological events, has become one of the most powerful lenses through which scientists at the Rocky Mountain Biological Laboratory (RMBL) understand how mountain ecosystems are responding to a warming climate. Because the growing season at high elevation is short and tightly bracketed by snowmelt and autumn frost, even small shifts in timing can cascade through plant reproduction, pollinator populations, and animal life cycles across the Gunnison Basin.
Several concepts are essential for understanding the findings that follow. Snow cover duration, the number of days the ground stays buried under snow, determines when plants can start growing and when ground-nesting bees can begin foraging. Frost damage occurs when freezing nights kill flower buds that have emerged too early, a risk that grows when snowmelt advances faster than the date of the last hard freeze. Phenological mismatch describes what happens when interacting species, such as a wildflower and the bumble bee that pollinates it, shift their timing at different rates and lose their synchrony. Related ideas include phenological overlap (how many weeks pollinators and flowers are both active), co-flowering patterns (which species bloom at the same time and compete or share pollinators), and the shape of the flowering curve (when bloom peaks, how long it lasts, and whether it is skewed early or late).
Tagged individual plants are monitored twice weekly throughout the growing season to record bloom start dates, bloom end dates, and total flower produ...
Shade cloths suspended 3m above treatment plots accelerate snowmelt by 5-7 days when snowpack reaches ~1m depth, simulating earlier spring snowmelt co...
Weekly monitoring of alpine plant flowering phenology coupled with snowmelt date recording to assess environmental effects on plant reproductive timin...
Statistical analysis using mixed effects models to evaluate relationships between plant clumping treatment and temperature responses while accounting ...
Long-term standardized sampling of aerial insects using a single Malaise trap at a fixed location operated weekly throughout growing seasons. Insects ...
Controlled factorial experiment manipulating both water availability and pollen supplementation to test for interactive effects on plant reproduction.
Harsh abiotic conditions–such as low temperatures that lead to spring and summer frost events in high-elevation and high-latitude ecosystems&nda...
Phenological advancements driven by climate change are especially pronounced at higher latitudes, so that migrants from lower latitudes may increasing...
1. Changes from historic weather patterns have affected the phenology of many organisms worldwide. Altered phenology can introduce organisms to novel ...
File: Peng_et_al._20206.zip Description: There are three folders here. The Data folder contains the raw specimen phenology data and the RMBL phenology...
We present infrastructure for developing large-scale and long-term phenological datasets across multiple herbaria, as well as a sample dataset that ha...
Prof. Rebecca (Becky) Irwin has been collecting data on the abundance and timing of bees in permanent sites near the Rocky Mountain Biological Lab (RM...
These concepts matter beyond academic interest. Wildflower displays, native bee populations, hummingbird migrations, and the timing of forage availability for elk and marmots all depend on the alignment of snow, sun, plants, and pollinators. As that alignment shifts, land managers and community members in the Gunnison Basin face questions about how meadows, pollinator services, and high-elevation biodiversity will look in the coming decades.
The foundation for this research area was laid by long-term observations begun in the 1970s near RMBL. Pleasants (Pleasants, 1980) demonstrated that subalpine plant species are organized into guilds that compete for shared bumble bee pollinators and that bloom in segregated sequences, an early indication that the timing of flowering is shaped by ecological interactions and not just climate. Price and Waser (Price & Waser, 1998) then used experimental overhead heaters to show that warming advances snowmelt and shifts plant reproduction earlier, especially for species that flower soon after snow disappears.
A turning point came when Inouye and colleagues (Inouye et al., 2000) reported that although spring temperatures were warming, snowmelt date at high elevation had not changed because of increased winter precipitation, while yellow-bellied marmots were emerging 38 days earlier and American robins were arriving 14 days earlier than two decades before. This was among the first clear demonstrations of altitudinal phenological mismatch. Inouye (Inouye, 2000) also articulated why frost matters: a single late freeze can kill an entire year's flower crop, with long-lasting consequences for perennial plants and the animals that depend on them. Forrest and Miller-Rushing (Forrest & Miller-Rushing, 2010) and Miller-Rushing and colleagues (Miller-Rushing et al., 2010) synthesized these threads, arguing that phenology connects individual physiology, population demography, and community interactions, and that specialist species with narrow active periods are especially vulnerable to mismatch.
Decades of monitoring have made one pattern unmistakable: at RMBL, the timing of snowmelt is the master variable. Inouye (Inouye, 2008) showed that earlier snowmelt is associated with earlier flowering in larkspur (Delphinium barbeyi) and exposes frost-sensitive buds of Helianthella quinquenervis to killing freezes, with mean bud frost damage rising from 36 percent in the 1990s to 74 percent from 1999 to 2006. Inouye (Inouye, 2022) confirmed that earlier snowmelt is strongly correlated with earlier flowering and longer growing seasons across many species. Snowmelt timing also affects which species bloom together: Forrest and colleagues (Forrest et al., 2010) found that in early-snowmelt years, the wildflower Lathyrus leucanthus overlapped with fewer co-flowering species, including a key pollinator-sharing partner. Aldridge and colleagues (Aldridge et al., 2011) documented that warmer summers have produced a bimodal flowering curve in subalpine meadows, with a mid-summer dip in floral abundance that did not exist in earlier decades.
These shifts ripple into pollinator populations. Boggs and Inouye (Boggs & Inouye, 2012) showed that snowmelt date drives population growth of the butterfly Speyeria mormonia both directly and indirectly through frost-mediated effects on nectar availability, together explaining 84 percent of variation in population growth. Ogilvie and colleagues (Ogilvie et al., 2017) demonstrated that interannual bumble bee abundance is driven mainly by the indirect effects of climate on floral resource timing, with snowmelt occurring nearly 13 days earlier over 43 years. Pyke and colleagues (Pyke et al., 2016) resurveyed bumble bees and plants 33 years after a 1974 census and found that flowering had shifted earlier while bumble bee phenology had not kept pace, reducing synchrony and bumble bee abundance, particularly at lower elevations. Thomson (Thomson, 2010) showed that the glacier lily Erythronium grandiflorum is becoming progressively poorly matched with its bumble bee pollinators over time, while McKinney and colleagues (McKinney et al., 2012) reported that broad-tailed hummingbirds and their early-season nectar plants are advancing at different rates.
Responses are not uniform across species or elevations. Inouye (Inouye, 2020) described how lower-elevation plants and shrubs are migrating upward, compressing alpine habitats and altering plant-pollinator networks. CaraDonna and colleagues (Iler et al., 2014) found that about 20 percent of species show nonlinear flowering responses, advancing only up to a threshold and then leveling off, suggesting some species are approaching biological limits on how much earlier they can flower.
Early work in the 1990s and 2000s established the basic correlations between snowmelt, flowering, and frost. Research since 2020 has shifted toward mechanism, multi-species comparison, and experimental manipulation. Prather and colleagues (Prather et al., 2023) analyzed 45 years of phenology data across plants, insects, birds, mammals, and an amphibian and showed that snowmelt advances phenology in every group, but that prior-season climate cues, sometimes lagged by up to two years, also play important roles. Dalton and colleagues (Dalton et al., 2023) reported a 47 percent decline in insect biomass and a 62 percent decline in insect abundance over 35 years in a protected subalpine meadow, linking the trend to drier winters and warmer summers. Stemkovski and colleagues (Stemkovski et al., 2023) examined the shape of phenological distributions, finding that both bees and flowers are right-skewed and that differences in skewness alone can change pairwise overlap by up to 14 percent.
New experimental work is dissecting the chain from snowmelt to seeds. Andrewlavage (Andrewlavage, 2025) extended phenology research from flowering into fruiting, finding that early snowmelt advanced fruiting time by six to eight days in several wildflowers but rarely changed total seed production. Sosa Antunez (Sosa Antunez, 2024) showed that early snowmelt reduced conspecific pollen deposition in Geum triflorum, and Rodelius and Iler (Rodelius & Iler, 2025) tested whether soil moisture and pollination jointly limit reproduction, finding little evidence for interactive effects. Goetting (Goetting, 2025) introduced plant pathogens into the picture, demonstrating that early snowmelt reduced rust infection on Linum lewisii. Uglialoro (Uglialoro, 2024) continued to track plant-hummingbird interactions, showing that broad-tailed hummingbirds begin feeding on key wildflowers as soon as they emerge, suggesting tight tracking but also vulnerability if flowers shift before birds arrive.
Many questions remain. How will mismatches accumulate over decades, and at what point do they translate into population declines for plants, pollinators, or migratory birds? Schmidt and colleagues (Iler et al., 2021) emphasized that few studies have yet connected phenological shifts to the specific vital rates that drive population trajectories. The mechanisms behind the recent insect declines documented by Dalton and colleagues (Dalton et al., 2023) are not fully resolved, and it is unclear whether they reflect local climate, regional drivers, or both. The role of microtopography in buffering or amplifying climate change, the potential for evolutionary adaptation in plant and pollinator phenology, and how upslope migration of lower-elevation species will reshape alpine communities all remain active frontiers. Finally, integrating long-term observational records with experimental manipulations, plant pathogen dynamics, and emerging questions about drought and precipitation variability will be central to forecasting the next decade of change in the Gunnison Basin.
Aldridge, G., Inouye, D., Forrest, J., Barr, W., Miller-Rushing, A. (2011). Emergence of a mid-season period of low floral resources in a montane meadow ecosystem associated with climate change. Journal of Ecology. →
Andrewlavage (2025). Impacts of earlier snowmelt on fruiting phenology and seed success of Rocky Mountain wildflowers. →
Boggs, C., Inouye, D. (2012). A single climate driver has direct and indirect effects on insect population dynamics. Ecology Letters. →
CaraDonna, P. et al. (2014). Nonlinear flowering responses to climate: are species approaching their limits of phenological change? →
Dalton, R. et al. (2023). Long-term declines in insect abundance and biomass in a subalpine habitat. Ecosphere. →
Forrest, J., Inouye, D., Thomson, J. (2010). Flowering phenology in subalpine meadows: does climate variation influence community co-flowering patterns? Ecology. →
Forrest, J., Miller-Rushing, A. (2010). Toward a synthetic understanding of the role of phenology in ecology and evolution. Philosophical Transactions of the Royal Society B. →
Goetting (2025). Prevalence and severity of Melampspora lini on Linum lewisii under early snowmelt conditions. →
Inouye, D. (2000). The ecological and evolutionary significance of frost in the context of climate change. Ecology Letters. →
Inouye, D. (2008). Effects of climate change on phenology, frost damage, and floral abundance of montane wildflowers. Ecology. →
Inouye, D. (2020). Effects of climate change on alpine plants and their pollinators. Annals of the New York Academy of Sciences. →
Inouye, D. (2022). Climate change and phenology. WIREs Climate Change. →
Inouye, D., Barr, B., Armitage, K., Inouye, B. (2000). Climate change is affecting altitudinal migrants and hibernating species. Proceedings of the National Academy of Sciences. →
McKinney, A. et al. (2012). Asynchronous changes in phenology of migrating Broad-tailed Hummingbirds and their early season nectar resources. →
Miller-Rushing, A., Hoye, T., Inouye, D., Post, E. (2010). The effects of phenological mismatches on demography. Philosophical Transactions of the Royal Society B. →
Ogilvie, J., Griffin, S., Gezon, Z., Inouye, B., Underwood, N., Inouye, D., Irwin, R. (2017). Interannual bumble bee abundance is driven by indirect climate effects on floral resource phenology. Ecology Letters. →
Pleasants, J. (1980). Competition for bumblebee pollinators in Rocky Mountain plant communities. Ecology. →
Prather, R. et al. (2023). Current and lagged climate affects phenology across diverse taxonomic groups. Proceedings of the Royal Society B. →
Price, M., Waser, N. (1998). Effects of experimental warming on plant reproductive phenology in a subalpine meadow. Ecology. →
Pyke, G., Thomson, J., Inouye, D., Miller, T. (2016). Effects of climate change on phenologies and distributions of bumble bees and the plants they visit. Ecosphere. →
Rodelius, K., Iler, A. (2025). Does pollination interact with the abiotic environment to affect plant reproduction? Annals of Botany. →
Schmidt et al. (2021). Demographic Consequences of Phenological Shifts in Response to Climate Change. →
Sosa Antunez (2024). How does early snowmelt affect pollen deposition on spring wildflowers? →
Stemkovski, M. et al. (2023). Skewness in bee and flower phenological distributions. Ecology. →
Thomson, J. (2010). Flowering phenology, fruiting success and progressive deterioration of pollination in an early-flowering geophyte. Philosophical Transactions of the Royal Society B. →
Uglialoro (2024). The Impact of Delphinium nuttallianum and Ipomopsis aggregata Phenology on Broad-tailed Hummingbird Visitation Patterns. →