00605nas a2200169   4500008004100000245012600041210006900167300001400236490000700250100002400257700001600281700002000297700001900317700002300336700001800359856005800377       2022                        eng d00aPrairie stream metabolism recovery varies based on antecedent hydrology across a stream network after a bank‐full flood0 aPrairie stream metabolism recovery varies based on antecedent hy  a1986-19990 v671 aRuffing, Claire, M.1 aVeach, A.M.1 aSchechner, Anne1 aRüegg, Janine1 aTrentman, Matt, T.1 aDodds, W., K.  uhttps://onlinelibrary.wiley.com/doi/10.1002/lno.1218203304nas a2200217   4500008004100000245012500041210006900166300001100235490000700246520259200253100001802845700002902863700001902892700002002911700001902931700002202950700002102972700001702993700002203010856005403032       2019                        eng d00aThe freshwater biome gradient framework: predicting macroscale properties based on latitude, altitude, and precipitation0 afreshwater biome gradient framework predicting macroscale proper  ae027860 v103 a<p>Understanding global ecological patterns and processes, from biogeochemical to biogeographical, requires broad‐scale macrosystems context for comparing and contrasting ecosystems. Climate gradients (precipitation and temperature) and other continental‐scale patterns shape freshwater environments due to their influences on terrestrial environments and their direct and indirect effects on the abiotic and biotic characteristics of lakes, streams, and wetlands. We combined literature review, analyses of open access data, and logical argument to assess abiotic and biotic characters of freshwater systems across gradients of latitude and elevation that drive precipitation, temperature, and other variability. We explored the predictive value of analyzing patterns in freshwater ecosystems at the global macrosystems scale. We found many patterns based on climate, particularly those dependent upon hydrologic characteristics and linked to characteristics of terrestrial biomes. For example, continental waters of dry areas will generally be widely dispersed and have higher probability of drying and network disconnection, greater temperatures, greater inorganic turbidity, greater salinity, and lower riparian canopy cover relative to areas with high precipitation. These factors will influence local community composition and ecosystem rates. Enough studies are now available at the continental or global scale to start to characterize patterns under a coherent conceptual framework, though considerable gaps exist in the tropics and less developed regions. We present illustrative global‐scale trends of abiotic, biotic, and anthropogenic impacts in freshwater ecosystems across gradients of precipitation and temperature to further understanding of broad‐scale trends and to aid prediction in the face of global change. We view freshwater systems as occurring across arrays of multiple gradients (including latitude, altitude, and precipitation) rather than areas with specific boundaries. While terrestrial biomes capture some variability along these gradients that influence freshwaters, other features such as, slope, geology, and historical glaciation also influence freshwaters. Our conceptual framework is not so much a single hypothesis as a way to logically characterize patterns in freshwaters at scales relevant to (1) evolutionary processes that give rise to freshwater biodiversity, (2) regulatory units that influence freshwater ecosystems, and (3) the current scope of anthropogenic impacts on freshwaters and the vital ecosystem services they provide.</p>1 aDodds, W., K.1 aBruckerhoff, Lindsey, A.1 aBatzer, Darold1 aSchechner, Anne1 aPennock, Casey1 aRenner, Elizabeth1 aTromboni, Flavia1 aBigham, Kari1 aGrieger, Samantha  uhttps://onlinelibrary.wiley.com/toc/21508925/10/7