Climate-change refugia can be defined by the strength of influence of physiographic and biotic properties on local atmospheric conditions relative to regional averages. In flatter landscapes, thermal heterogeneity and decoupling may be limited. We sought to quantify the magnitude of climate decoupling produced by topographic variation and vegetation in North America's boreal-parkland-grassland transition zone. We deployed iButton data loggers at four hill and 12 river valley systems along a latitudinal gradient in Alberta, Canada (N = 240) between 2014 and 2018. We modelled monthly temperature metrics by season as a function of topography and percent vegetation cover using general linear mixed effect models. Summer Tmax varied ~6 oC acros...
Climate change is projected to dramatically increase boreal wildfire activity, with broad ecological...
The majority of microclimate studies have been done in topographically complex landscapes to quantif...
Graduation date: 1993Presentation date: 1992-10-28The equilibrium response of Canadian vegetation to...
Climate warming leads to vast changes in the land cover types and plant biomass in the northern high...
High precipitation in boreal northeastern North America could help forests withstand the expected te...
1.Tall-shrub expansion into low-statured communities, a hallmark of recent vegetative change across ...
Global temperature is increasing, especially over northern lands (>50 degrees N), owing to positi...
The boreal forest circles the high northern latitudes but it is far from a continuous carpet of ever...
Grasslands hold varied grazing capacity, provide multiple habitats for diverse wildlife, and are a k...
In order to estimate the effect of drastic land use changes on the global mean temperature, a set of...
Vegetation productivity across the boreal forest has increased over the past several decades. Howeve...
Synthesis of results from several Arctic and boreal research programmes provides evidence for the st...
Amplified warming at high latitudes over the past few decades has led to changes in the boreal and A...
Understanding the sensitivity of tundra vegetation to climate warming is critical to forecasting fut...
Climate models simulating continental scale deforestation suggest a warming effect of land clearing ...
Climate change is projected to dramatically increase boreal wildfire activity, with broad ecological...
The majority of microclimate studies have been done in topographically complex landscapes to quantif...
Graduation date: 1993Presentation date: 1992-10-28The equilibrium response of Canadian vegetation to...
Climate warming leads to vast changes in the land cover types and plant biomass in the northern high...
High precipitation in boreal northeastern North America could help forests withstand the expected te...
1.Tall-shrub expansion into low-statured communities, a hallmark of recent vegetative change across ...
Global temperature is increasing, especially over northern lands (>50 degrees N), owing to positi...
The boreal forest circles the high northern latitudes but it is far from a continuous carpet of ever...
Grasslands hold varied grazing capacity, provide multiple habitats for diverse wildlife, and are a k...
In order to estimate the effect of drastic land use changes on the global mean temperature, a set of...
Vegetation productivity across the boreal forest has increased over the past several decades. Howeve...
Synthesis of results from several Arctic and boreal research programmes provides evidence for the st...
Amplified warming at high latitudes over the past few decades has led to changes in the boreal and A...
Understanding the sensitivity of tundra vegetation to climate warming is critical to forecasting fut...
Climate models simulating continental scale deforestation suggest a warming effect of land clearing ...
Climate change is projected to dramatically increase boreal wildfire activity, with broad ecological...
The majority of microclimate studies have been done in topographically complex landscapes to quantif...
Graduation date: 1993Presentation date: 1992-10-28The equilibrium response of Canadian vegetation to...