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2,322 results for “precipitations”
Figure S29 in Supplementary Materials for Precipitation is the main axis of tropical plant phylogenetic turnover across space and time
Figure S29 (lef). Chloroplast gene tree for Caesalpinioideae based on analysis of 72 plastid genes using RAxML. All nodes have maximal bootstrap support except those labelled with actual support values <100%.
Figure S13 in Supplementary Materials for Precipitation is the main axis of tropical plant phylogenetic turnover across space and time
Figure S13 (lef).'oot-to-tip length variances per gene tree. The cut-off of 0.009 is indicated with a dashed vertical line.
Figure S26 in Supplementary Materials for Precipitation is the main axis of tropical plant phylogenetic turnover across space and time
Figure S26. Tanglegram comparing the ASTRAL single-copy genes phylogeny (Figure S14) with the PhyloBayes phylogeny (Figure S23).
Figure S23 in Supplementary Materials for Precipitation is the main axis of tropical plant phylogenetic turnover across space and time
Figure S23. Phylogeny of Caesalpinioideae. PhyloBayes species tree. Posterior probability support values are only shown for nodes with a posterior probability <1.
Figure S10 in Supplementary Materials for Precipitation is the main axis of tropical plant phylogenetic turnover across space and time
Figure S10 (lef). Numbers of genes with potential paralogs per sample. The eleven samples with the most potential paralogs are labelled.
Figure S25 in Supplementary Materials for Precipitation is the main axis of tropical plant phylogenetic turnover across space and time
Figure S25. Tanglegram comparing the ASTRAL single-copy genes phylogeny (Figure S14) with the RAxML amino acid single-copy genes phylogeny (Figure S20).
Figure S28 in Supplementary Materials for Precipitation is the main axis of tropical plant phylogenetic turnover across space and time
Figure S28. Levels of topological congruence between phylogenies generated in different ways, estimated as Robinson-Foulds (RF) distances between species trees. Exact values are in Table S17. Thickness of the connecting lines reflects RF distance. Abbreviations are as follows 'AS' = ASTRAL-3; 'RA' = RAxML; '997' = all genes without paralogs, '997p'= all genes with paralogs, 'SC' = single-copy genes; 'NT' = nucleotide alignment; 'AA' = amino acid alignment; 'PB' = PhyloBayes phylogeny; 'CP' = chloroplast phylogeny.
Figure S40 in Supplementary Materials for Precipitation is the main axis of tropical plant phylogenetic turnover across space and time
Figure S40. Phyloregionalization of Australia using the metachronogram. Subfigures show clustering results with two to eight phyloregions, as well as the results of phyloregionalization analyses using the geographic residuals of phylogenetic turnover, and ancient phylogenetic turnover with a cut-off of 5, 10, and 20 million years.
Figure S44 in Supplementary Materials for Precipitation is the main axis of tropical plant phylogenetic turnover across space and time
Figure S44. Phyloregionalization per continent using the genus-level Mimosoid phylogeny (rather than the metachronogram). Caption otherwise as for Figure 3.
Figure S41 in Supplementary Materials for Precipitation is the main axis of tropical plant phylogenetic turnover across space and time
Figure S41. Phyloregionalization of the global tropics using the metachronogram. Subfigures show clustering results with two to eight phyloregions, as well as the results of phyloregionalization analyses using the geographic residuals of phylogenetic turnover, and ancient phylogenetic turnover with a cut-off of 5, 10, and 20 million years.
Figure S39 in Supplementary Materials for Precipitation is the main axis of tropical plant phylogenetic turnover across space and time
Figure S39. Phyloregionalization of Asia using the metachronogram. Subfigures show clustering results with two to eight phyloregions, as well as the results of phyloregionalization analyses using the geographic residuals of phylogenetic turnover, and ancient phylogenetic turnover with a cut-off of 5, 10, and 20 million years.
Figure S32 in Supplementary Materials for Precipitation is the main axis of tropical plant phylogenetic turnover across space and time
Figure S32 (lef). Internode certainty values based on the 821 single-copy gene trees mapped onto the single-copy genes ASTRAL species tree (Figure S14). For each node, the upper number shows the quartet-based Extended Quadripartition Internode Certainty (EQP-IC) score calculated with QuartetScores, and the lower number shows the bipartition-based Internode Certainty All score calculated with PhyParts, both rounded down to two digits. Boxes are coloured based on unrounded values: green for values ≥ 0.5, yellow for values ≥ 0 and <0.5, and red for values <0. Branch lengths are set equal for easier visualisation. Inset depicts a correlation plot between the two measures.
Figure S33 in Supplementary Materials for Precipitation is the main axis of tropical plant phylogenetic turnover across space and time
Figure S33 (right).'esults of ASTRAL's polytomy test based on the 821 single-copy gene trees mapped onto the single-copy genes ASTRAL species tree (Figure S14). Node numbers are tests of the null hypothesis that a branch should be replaced by a polytomy. Only node numbers> 0.05 are shown. Branch lengths are set equal for easier visualisation.
Figure S31 in Supplementary Materials for Precipitation is the main axis of tropical plant phylogenetic turnover across space and time
Figure S31. Gene tree incongruence mapped onto the time-calibrated version of the phylogenomic backbone of Caesalpinioideae. Each branch is coloured to reflect the ratio of total supporting versus total conflicting gene trees as determined by PhyParts. Clades named by Koenen et al. (24) are labelled. Two recent radiations in Madagascar, one in the Dichrostachys clade and one in Albizia, are highlighted.
Figure S36 in Supplementary Materials for Precipitation is the main axis of tropical plant phylogenetic turnover across space and time
Figure S36. Phyloregionalization of North America using the metachronogram. Subfigures show clustering results with two to eight phyloregions, as well as the results of phyloregionalization analyses using the geographic residuals of phylogenetic turnover, and ancient phylogenetic turnover with a cut-off of 5, 10, and 20 million years.
Figure S14 in Supplementary Materials for Precipitation is the main axis of tropical plant phylogenetic turnover across space and time
Figure S14. Phylogeny of Caesalpinioideae. ASTRAL species tree based on the 821 single-copy gene trees. Local posterior probability support values are only shown for nodes with a local posterior probability <1. Branch lengths are expressed in coalescent units. Terminal branches were assigned an arbitrary uniform length for visual clarity.
Fig. 2 in Precipitation is the main axis of tropical plant phylogenetic turnover across space and time
Fig. 2. Drivers of phylogenetic turnover of Mimosoid legumes across the global lowland tropics. Bars show relative fractions of phylogenetic turnover explained by predictors (rescaled to add up to one). Numbers above bars are absolute explained percentages of turnover (tables S12 and S20). (A) Phylogenetic turnover explained by climatic distance (maroon), geographic distance (blue), or their interaction (cream). Turnover is assessed across four depths in the phylogeny: with the full metachronogram (age cutoff of 0) and with all clades younger than 5, 10, and 20 Ma collapsed. Note that it was not possible to fit a model to the phylogeny collapsed at 20 Ma for the pantropical and Australian models. (B) Phylogenetic turnover explained by MAP (green) and/or annual mean temperature (orange). Turnover is expressed as phylogenetic turnover not explained by geographic distance ("geographic residuals"). (C) Geographic residuals of phylogenetic turnover explained by MAP (green) and/or precipitation seasonality (gray; left) or dry season length (DSL) (i.e., the number of consecutive months with precipitation <100 mm/month; yellow; right). See fig. S45 for results obtained with an alternative, genus-level Mimosoid phylogeny. P, MAP; T, annual mean temperature; Pseas, precipitation seasonality.
Fig. 1 in Precipitation is the main axis of tropical plant phylogenetic turnover across space and time
Fig. 1. Mimosoid evolution and diversity across precipitation gradients. (A) Phylogeny of Mimosoid legumes showing the evolution of precipitation niches and transcontinental dispersal events through time. Branch colors correspond to mean annual precipitation (MAP) estimates [see (C) for scale]. Pie charts at tips and nodes of named clades [sensu (24)] represent observed and estimated spatial distributions [based on area definitions in (D)]. Ancestral niches and areas were estimated using a complete metachronogram for Caesalpinioideae, including non-Mimosoid Caesalpinioideae taxa, but only the Mimosoid clade is shown here. Green circles on branches indicate shifts between precipitation categories [following (17)] that encompass a difference of at least 250-mm MAP; red triangles indicate postulated transcontinental dispersals according to the best-supported model. The six most species-rich genera are labeled. (B) Fractions of niche shifts and transcontinental dispersal events, averaged across multiple optimizations, relative to total phylogenetic splits plotted through time for 5-Ma bins. (E) Mimosoid growth form diversity across the tropical precipitation gradient, from deserts with <50-mm MAP (left) through savannas to rain forests with>5000-mm MAP (right). See the Supplementary Results for species names and photographers. See fig. S51 for more information.
STEAM evaporation and precipitation for potential vegetation and current land use scenarios
<p>This dataset contains global evaporation and precipitation data generated and described in the following research article:</p> <p><strong>Wang-Erlandsson, L., Fetzer, I., Keys, P. W., van der Ent, R. J., Savenije, H. H. G., and Gordon, L. J.: Remote land use impacts on river flows through atmospheric teleconnections, Hydrol. Earth Syst. Sci., 22, 4311–4328, https://doi.org/10.5194/hess-22-4311-2018, 2018.</strong></p> <p>The dataset includes evaporation and precipitation for a potential vegetation (pv) and a current land use scenario (cur) and comes in monthly resolution and a spatial grid of 1.5° over the period 2000 - 2013. The files are saved in MAT file format.</p> <p>In addition, it includes the data in NetCDF files regridded using cdo (remapnn) to 0.5° spatial resolution.</p>
Increased precipitation over land due to climate feedback of large-scale bioenergy cultivation
<p>Biophysical effects of different bioenergy crop cultivation scenarios on global water cycles simulated by coupled IPSL-CM model, with ORCHIDEE-MICT-BIOENERGY as the land component and LMDz as the atmosphere component. The spatial resolution of the coupled model was 1.26° latitude × 2.5° longitude (i.e., 143*144 grid cells globally).</p> <p>Datasets includes:</p> <p>1. Source data and plotting code for Figure 1, the global precipitation changes induced by bioenergy cultivation.</p> <p>2. Source data and plotting code for Figure 2, the diagnostic precipitation changes for global land area, in and outside of the bioenergy cultivation area.</p> <p>3. Source data plotting code for Figure 3, the changes in water balance for global land area, in and outside of bioenergy cultivation area, monsoon regions and four different humidity zones.</p>
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