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from the modelling, the greatest contribution to provision was from upstream natural and semi-natural ecosystems with high capacity and high downstream demand. however, only a small proportion of canada’s freshwater is supplied through these channels. about two-thirds of the freshwater supply in canada comes from runoff of precipitation over land, which is distributed across the country’s watersheds. we identified canada’s 20 best watersheds for freshwater provision, which were associated with about 2.8 billion m3of freshwater production in 2017. the majority of these watersheds were found in the boreal and forested provinces of ontario and quebec, but also within the saskatchewan grain belt and the alberta pastureland plains. in these watersheds, natural or semi-natural ecosystems, such as lakes, wetlands, and prairie land, with high capacity and high downstream demand were critical for freshwater provision. in fact, a large proportion of these ecosystems in ontario and quebec are currently impaired by some level of water quality impairment, highlighting the need to protect them from degradation.
We quantified climate regulation capacity by calculating the total amount of carbon stored above- and belowground in each pixel across Canada. Aboveground carbon data came from the Canadian National Forest Inventory (Gillis et al 2005, Beaudoin et al 2014 ) datasets of total live aboveground biomass (branch, foliage, stem bark, and stem wood) and total dead biomass from 2015 (figures A1(a) and (b) (available online at )). We estimated aboveground carbon by assuming that carbon makes up 48% of the aboveground biomass present (Asner et al 2010 ). Belowground carbon estimates were obtained from the 2017 SoilGrids system (Hengl et al 2014 ) dataset that provides soil organic carbon content from 0 m to 1 m depth (figures A1(c) and (d)). We then summed these pixel-level estimates of aboveground and belowground carbon to obtain total carbon store values and then normalized (i.e. min-max scaled) these values between 0 and 1 to calculate relative climate regulation importance. Because carbon stored at any location meets demand for climate regulation globally via atmospheric mixing (Costanza 2008 ), we assumed global flow of benefits from stored carbon and quantified service provision solely as capacity (i.e. carbon storage).
For freshwater, we quantified capacity as the modelled total amount of annual freshwater runoff. We used the cumulative freshwater flow from either the forested watershed layer (i.e. forested lands with greater than 30% cover), the agricultural watershed layer (i.e. lands with less than 30% cover and areas with some runoff), or the cropland layer (i.e. lands with less than 30% cover but a higher than 15% share of anthropogenic water consumption) as potential capacity. We defined demand as the cumulative water consumption (in litres) from four principal beneficiary sectors: municipal, commercial, residential, and industrial (i.e. industrial = factories and thermal power stations). As the vast majority of Canadians live in urbanized areas, we assumed all freshwater demand is municipal in nature (StatCan 2013 ). We calculated demand for the same four sectors as used for capacity as proxies for the freshwater capacity of natural locations, i.e. land areas that supply water or are sensitive to water consumption, including wetlands (Belyea et al 2009 ), unconsolidated glacial deposits (Belyea et al 2005 ), and other (i.e. no capacity or high consumption), similar to the analysis conducted by Watson et al (2014). Demand values were scaled to represent the relative amount of water consumed in the four sectors, comparing current estimates across Canada to the estimates under future conditions for the amount of water withdrawn in the future, as estimated by the most recent CCSP (United Nations 2016).
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