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1  to differential acclimating behaviors under drought.
2 s may have modified Delta(13) C responses to drought.
3 etition caused rank changes in fitness under drought.
4 pportunities to improve our understanding of drought.
5 redictions of delayed-mortality responses to drought.
6 ble of enhancing rice growth during moderate drought.
7 n about plant performance and survival under drought.
8 -regulated poplar root growth in response to drought.
9 and microbes during, and particularly after, drought.
10 chitecture of gene expression in response to drought.
11  presence in areas that experienced postfire drought.
12 ima were separated by a period of foresummer drought.
13 ich plants were subjected to three cycles of drought.
14 all vascular plants, have few adaptations to drought.
15 g landscape irrigation, during the 2012-2016 drought.
16 ferent forms of stress, especially shade and drought.
17 >30 m) groundwater performed best during the drought.
18 al stresses such as extreme temperatures and drought.
19 n at eight out of the 10 forest sites during drought.
20 ) ) are critical to a species' adaptation to drought.
21 States, when controlling for temperature and drought.
22 ential to increase crop resilience to future drought.
23  instrumental record including the Dust Bowl drought.
24 ce of root exudates in ecosystem response to drought.
25 p = 0.001) compared with those not living in drought.
26  trophic mismatch with the green wave during drought.
27 gnificant tree mortality than the Millennium drought.
28 ee size and traits shape growth responses to droughts.
29  and intense heat waves, storms, floods, and droughts.
30 o experience hydraulic failure during severe droughts.
31 f global warming and increasing frequency of droughts.
32 nomic risks of cooling water shortage during droughts.
33 roughts in the historical record (Millennium Drought, 2000-2009 and Big Dry, 2017-2019).
34 Serbia in maize growing seasons with extreme drought (2012), extreme precipitation and flood (2014) a
35 pitation (+73.1%) but inhibited by increased drought (-30.4%), N deposition (-31.0%), and combination
36 ect of microplastics (i.e., microfibers) and drought, a factor with which microfibers might interact,
37 CE investigations of the value of traits for drought adaptation to be conducted under more severe dro
38 insights into plant habitat distribution and drought adaptation.
39 o Amazonian tropical forests and can, during drought, affect larger areas than deforestation itself.
40  and vegetation dynamics, and focuses on how drought affects interactions between conifer trees and b
41 eficial soil microbial communities, and that drought affects the quantity and quality of root exudati
42 the reservoir fills; and a severe multi-year drought after the filling.
43  migratory route, mule deer closely followed drought-altered green waves during migration.
44 tic sample, 10.7% (9,019) experienced severe drought and 23.4% (19,639) experienced mild/moderate dro
45 ese differences in vulnerability to climatic drought and climate change.
46                                   We imposed drought and competition treatments on diverse genotypes.
47 d-use change act synergistically, increasing drought and fire frequencies, converting several tropica
48 s in external morphology and wood anatomy to drought and fire were similar to those of some modern tr
49 years, we evaluated the effects of a natural drought and in situ experimental warming on density-depe
50 ttle is known about the relationship between drought and intimate partner violence (IPV).
51 red hypothesized mediating variables linking drought and IPV, prohibiting a formal mediation analysis
52 ing the statistics, physics, and dynamics of drought and its causes in a historical context.
53  Estimates were up to 21% and 4% higher when drought and O(3) stress were neglected respectively.
54                        With the inclusion of drought and O(3) stress, GPP at CPZ, BLO and HYY is proj
55  for expanding water security in the face of drought and other water hazards.
56                    With a 19 year dataset on drought and plant phenology across 99 unique migratory r
57 neous selection has higher correlations with drought and plant productivity under warming than contro
58                              Under prolonged drought and reduced photosynthesis, plants consume store
59 oupled with fine root growth dynamics during drought and return of soil moisture.
60                Hyperosmotic stress caused by drought and salinity is a significant environmental thre
61                  Abiotic stresses, including drought and salinity, trigger a complex osmotic-stress a
62 at occurred in California following a 4-year drought and widespread pest outbreaks.
63 utheast Asian region following unprecedented drought and wildfires.
64 tion, these events have been linked to flash droughts and can play a critical role in the spread of h
65 ican (SA) societies are highly vulnerable to droughts and pluvials, but lack of long-term climate obs
66 gest SA will experience more frequent/severe droughts and rainfall events as a consequence of increas
67 eb dynamics in coastal and shelf areas where droughts and stratification lead to increasing nutrient
68        Here we show that increasingly severe droughts and temperature driven reductions in growing se
69 ntially expressed during pathogen infection, drought, and abscisic acid treatment.
70 understanding of g(s) dynamics over seasonal drought, and identifies a practical, trait-based approac
71 ationship between rain, extreme rain, flood, drought, and season (rainy vs. dry) and diarrheal illnes
72 ich species and trees are most vulnerable to drought, and the underlying mechanisms have remained elu
73  CEs potentially causing high-impact floods, droughts, and fires.
74 is-element in intronic poly(A) sites used in drought- and heat-stressed plants that might play an imp
75 ategies affected species responses to severe drought; and how potential rooting depths varied across
76 a's 2019-2020 mega-fires were exacerbated by drought, anthropogenic climate change and existing land-
77                    Robust shifts in seasonal drought are most apparent during the cool season; when s
78 scale assessments of vegetation responses to drought are needed to anticipate, manage, and potentiall
79 nges in precipitation, changes in ecological drought are robust over large portions of drylands in th
80                                    Extensive droughts are consistent with the observed 20th-century t
81 which are becoming as severe and frequent as droughts, are overlooked and their impacts remain poorly
82    With California's 2013-2016 extraordinary drought as a natural experiment, we studied four co-occu
83 f permeability in maize seedlings exposed to drought as well as abscisic acid treatment, which implie
84 ochemical processes; however, no global snow drought assessments currently exist.
85 PRLT2/89-33 has an inherent ability to sense drought at both developmental stages.
86 nces our understanding of plant responses to drought at regional scales.
87 scPDSI) dataset to derive the South American Drought Atlas (SADA) over the continent south of 12 degr
88 sponse to drought events: those dominated by drought-avoiding species showed strong covariance betwee
89  precipitation and increased temperature and drought, bar-built estuaries have transitioned from loti
90                            We find that snow droughts became more prevalent, intensified, and lengthe
91 nt stresses, such as nutrient deficiency and drought, before the onset of visible symptoms and subseq
92 -driven risks to forest stability from fire, drought, biotic agents, and other disturbances.
93                      We found no evidence of drought-buffered routes.
94 ears transition into ecological traps during drought but also highlight that some pools serve as refu
95 ty level, shoot and root mass decreased with drought but increased with microfibers, an effect likely
96  is related to the ability to survive future droughts by using a tree-ring database of surviving and
97 our experiment suggests that even short-term droughts can have extended consequences for stream ecosy
98 ikely contribute to observed changes in snow drought characteristics.
99               Extreme climate events such as droughts, cold snaps, and hurricanes can be powerful age
100                         We observed genotype-drought-competition interactions for relative fitness: c
101  precipitation and flood (2014) and moderate drought conditions (2013 and 2015).
102       The latter seems to be essential under drought conditions and explains the intense occurrence o
103 adaptation to be conducted under more severe drought conditions and variable timing of drought stress
104 nts of 1983, 1997/98 and 2015/16, indicating drought conditions with less river runoff, rainfall and
105 lone criterium for quantifying and reporting drought conditions.
106 me pools serve as refuges even under extreme drought conditions.
107  that described in modern trees experiencing drought conditions.
108 s, ranging from frequent downpours to severe droughts, could cause widespread, but largely unknown, a
109                                   In neither drought did CABLE predict that trees would have reached
110 ether embolism formation in the xylem during drought drives this leaf mortality.
111 rsal also altered soil community response to drought; drought had a stronger effect on bacterial (but
112 olling the gene expression constitutively or drought-dynamically are unraveled.
113  has increasingly influenced the severity of drought events by decreasing runoff efficiency in the ba
114 exico, provide unambiguous evidence for five drought events that impacted the Ancestral Puebloan soci
115 data has been widely used for characterizing drought events.
116 e carbon carrying capacity adjusts to severe drought events.
117           Forest types varied in response to drought events: those dominated by drought-avoiding spec
118 moisture recycling and resulted in increased drought extent and severity, and subsequent fire.
119 en weeks, resulting in disruptive heatwaves, droughts, flooding, snowfalls, and cold spells.
120 igher basin-wide precipitation and increased drought frequency and severity.
121  concentrations, coupled with an increase in drought frequency due to climate change, pose a threat t
122 unities are discussed for new innovations in drought gene discovery using platforms targeting the ext
123 reduced recovery (low capacity to attain pre-drought growth rates) in gymnosperms.
124  altered soil community response to drought; drought had a stronger effect on bacterial (but not fung
125                Women living in mild/moderate drought had higher risk of reporting physical (marginal
126 ritical trait for predicting survival during drought, had highly species-specific responses: in one s
127          The loss of stable coexistence when drought has different effects on the competing aphid phe
128 we show that tree mortality concomitant with drought has led to short-term (mean 5 y, range 1 to 23 y
129                                              Drought has many known deleterious impacts on human heal
130                                              Drought has promoted large-scale, insect-induced tree mo
131 d mortality and community dynamics following drought have major ecological and societal impacts.
132 tural and demographic impacts of a series of droughts have primarily been developed from the environm
133 isturbance, largely during periods of severe drought, have affected as much of the forest area in the
134  occurrence of APA in Sorghum in response to drought, heat, and salt stress.
135 Each year, abiotic stress conditions such as drought, heat, salinity, cold and particularly their dif
136 the responses of 20-53 species to an extreme drought in a seasonally dry tropical forest in Costa Ric
137 a (SSA) resulted in the Cape Town "Day Zero" drought in early 2018.
138           As climate change drives increased drought in many forested regions, mechanistic understand
139  belowground microbial community response to drought in temperate maize agroecosystems, as well as ho
140           The evidence indicates a prolonged drought in the likely western source region for these co
141  period included the recent, severe regional drought in the western United States (2012-2016).
142 and 23.4% (19,639) experienced mild/moderate drought in the year prior to the survey, with substantia
143 ere is a consensus about negative impacts of droughts in Amazonia.
144  recently been subjected to two of the worst droughts in the historical record (Millennium Drought, 2
145  We assessed how growth resilience to severe droughts, including its components resistance and recove
146 [CO(2) ], increased precipitation, increased drought, increased N deposition, and their combinations)
147                Climatic factors, such as the drought index and growing degree days (GDD), had a signi
148  climate, chiefly median Palmer Hydrological Drought Index and other aridity metrics.
149 SDI exhibits consistency with meteorological drought indices in both basins.
150 ivity measurements (Lp(r) ), we examined how drought-induced changes in anatomy and hydraulic propert
151                                          The drought-induced decrease in NEP, which mostly occurred i
152 any ATPases) completely halted recovery from drought-induced embolism for up to 24 h after re-irrigat
153 now little about its ability to recover from drought-induced embolism.
154 make regional-scale predictions of potential drought-induced hydraulic failure.
155  there is a large variation in the degree of drought-induced leaf death across the canopy, to test wh
156 ease under anthropogenic climate change, and drought-induced mortality and community dynamics followi
157  determining the physiological mechanisms of drought-induced mortality in woody plants and identifyin
158 vel models that simulate the carbon costs of drought-induced plant hydraulic failure are improving pr
159 arming had few direct effects, but amplified drought-induced reductions in whole-tree g(m) .
160 the petiole strongly correlated with area of drought-induced tissue death in individual leaves.
161  As a physical response to water loss during drought, inner Selaginella lepidophylla stems curl into
162  with fluvial entrenchment during periods of drought, instead of being related to destructive invasio
163                    As climate change-induced droughts intensify, tall trees with drought-sensitive le
164                                              Drought is a critical stressor that contributes to water
165 o too do the effects of environment, as when drought is amplified by competition.
166                      Forest vulnerability to drought is expected to increase under anthropogenic clim
167           The capacity of trees to withstand drought is likely to be determined by traits associated
168 ence is rising that its resilience to severe drought is limited.
169                                              Drought is one of the main constraints in peanut product
170 rn United States during periods of prolonged droughts is poorly understood as regional hydroclimate r
171 unities experience more frequent and extreme droughts, it is increasingly important that water suppli
172 xperienced decreases in occurrence following drought-like conditions, while widespread species were u
173  of identifying robust changes in ecological drought may be useful for other assessments of climate i
174                                              Drought mortality increased dead tree and surface fuel c
175     Additionally, we analyzed the effects of drought- mortality on second-entry burn emissions and co
176 s the Upper Missouri River Basin, the recent drought of 2000 to 2010, known as the "turn-of-the-centu
177             We investigated the responses to drought of key fitness-related traits such as stomatal r
178                                              Droughts of the future are likely to be more frequent, s
179 m experiment, we investigated how impacts of drought on boreal stream ecosystems are altered by the s
180 tance may have underestimated the impacts of drought on gymnosperm-dominated forests under future cli
181  successional forests have been resilient to drought over the past 18 years, from the perspective of
182 studies have combined FACE with temperature, drought, ozone, and nitrogen treatments.
183 draulic conductivity and dye staining during drought progression and short-term (2 d) and long-term (
184 , they have not been as widely used in other drought-prone regions throughout the rest of the world,
185  species-specific mortality rates during the drought ranged from 0% to 34%, and varied little as a fu
186                                              Drought reduced whole-tree g(m) .
187                              In angiosperms, drought-related mortality risk is associated with lower
188                                              Drought-related tree mortality is now a widespread pheno
189 cent reduction in vegetation greenness under droughts relative to baseline moisture conditions.
190 s were less resilient to previous non-lethal droughts, relative to coexisting surviving trees of the
191                                    Following drought release, we found a gradual recovery of leaf gas
192 an adjust hydraulic traits when experiencing drought remain rare.
193 ter deficits (e.g., mild, moderate or severe drought) remain elusive.
194 nagers, early career scientists, and veteran drought researchers will likely see opportunities to imp
195 neer improved water-use efficiency (WUE) and drought resilience in C(3) plants while sustaining produ
196                               In particular, drought resilience markedly increased, but resistance de
197 osperms showed different spatial patterns of drought resistance and resilience, driven by variations
198 nt nf-yb21 exhibited reduced root growth and drought resistance.
199 , which ultimately increased root growth and drought resistance.
200 nd provides insights relevant to breeding of drought-resistant crops.
201                                       From a drought-resistant cultivar of Oryza sativa (rice), we is
202                   Additionally, differential drought response among retained paralogous pairs suggest
203 oles of CDK8 in modulating ABA signaling and drought responses.
204 the coevolution of the EDS1/PAD4 pathway and drought responses.
205 N is required for HSFA6a to regulate ABA and drought responses.
206 ing early generation selection for selecting drought-responsive genotypes.
207                             While 12% of the drought-responsive transcripts have similar dynamics in
208 itannins with antimicrobial properties under drought reveals an adaptive response by fine roots to pr
209  two lavender species exposed to a series of drought/rewatering cycles that varied in drought-stress
210 g than they have been in recent decades, but drought risks will be lower if greenhouse gas emissions
211 ption of various abiotic stresses, including drought, salinity, flooding, and temperature stress.
212 um experimental system that compares between drought-sensitive (ICSB338) and enhanced drought-toleran
213 -induced droughts intensify, tall trees with drought-sensitive leaves will be most vulnerable to imme
214 ant variety, but recovery is impaired in the drought-sensitive sorghum variety.
215                            We quantified the drought sensitivity of vegetation in the Pacific Northwe
216                      However, variability in drought sensitivity was considerable within biomes and w
217        We found that in addition to climatic drought severity (i.e., rainfall), subsurface processes
218 e this network with a self-calibrated Palmer Drought Severity Index (scPDSI) dataset to derive the So
219 stream habitats, a consequence of increasing drought severity.
220 ungulates to surf, little is known about how drought shapes the green wave and influences the foragin
221 western Wyoming, United States, we show that drought shortened the duration of spring green-up by app
222 mmediate transcriptional response to ABA and drought signals.
223          Differential miRNA expression among drought specific tissues indicted the probable energy co
224 ach of 15 years, data were based on reported drought status for August, wetland cover, the physiograp
225  SCA at MLO is mainly exerted by intensified drought stress acting to offset the acceleration driven
226 elevated temperatures, CO(2) concentrations, drought stress and nutrient conditions directly and indi
227 ips1 (nut1), that mimics tassel blasting and drought stress and reveals the genetic mechanisms underl
228  of comparative transcriptome analysis under drought stress at two different developmental stages whi
229 l the study sites was obtained with O(3) and drought stress combined, such that the two stressors cou
230 ere was some evidence that the timing of the drought stress during crop growth influenced the effect
231 s, using our existing data on the effects of drought stress in crops as an example.
232 nnual plants, higher temperatures, CO(2) and drought stress increase foliar herbivory.
233 ly, we find no signal for stochasticity when drought stress is relieved, likely due to renewed select
234                              When exposed to drought stress many plants reprogram their gene expressi
235                                     We found drought stress was the more significant as it reduced mo
236 re drought conditions and variable timing of drought stress, a risky but necessary endeavour.
237 ghum was shaped by diversifying selection on drought stress, and can inform genomics-enabled breeding
238 ent physiological changes to mild and severe drought stress, and the associated transcriptome dynamic
239 ays an important role in plant adaptation to drought stress, but the underlying molecular mechanisms
240 further reflects pressures to avoid frost or drought stress.
241 d stomatal apertures and hypersensitivity to drought stress.
242 how forest carbon fluxes respond to heat and drought stress.
243  in rice roots and is strongly responsive to drought stress.
244 tolerant genotype, PRLT2/89-33, subjected to drought stress.
245  a C(4) herb capable of performing CAM under drought stress.
246  of drought/rewatering cycles that varied in drought-stress intensity.
247 arly in host development and when sorghum is drought stressed, conditions when mycobiomes are small.
248  almeriense mycorrhiza from well-watered and drought-stressed plants, when intracellular colonization
249     This failure to adjust resulted in these drought-stressed trees experiencing significantly lower
250 traits relating to plant hydraulic stress in drought-stressed trees.
251 mers had traits conferring more tolerance to drought such as small sclerophyllous leaves and lower pe
252 n woody plants and identifying thresholds of drought survivorship will improve forecasts of forest an
253 ent, lower reproductive potential and higher drought susceptibility.
254 ental stage in fine roots of 101-14Mgt (i.e. drought susceptible), probably limiting cortical lacunae
255 thin protected forests was more resilient to drought than within non-protected forests.
256 mber of foliar functional traits affected by drought that can be used as indicators of plant water st
257     Our study revealed that, when exposed to drought, the composition of heteropolymers are strategic
258             Cassava is cultivated due to its drought tolerance and high carbohydrate-containing stora
259            Clusters associated with improved drought tolerance consisted of phene states that likely
260 ction and leading to greater WUE(i) provides drought tolerance in Caragana species adapted to low-MAP
261 stic understanding of the factors conferring drought tolerance in trees is increasingly important.
262  At present, the molecular basis of terminal drought tolerance of certain pearl millet genotypes rema
263                     Two proteins involved in drought tolerance were also identified.
264 y and environmentally relevant traits (e.g., drought tolerance); however, incorporating high-dimensio
265 d, while knockdown of ZmPTPN inhibited plant drought tolerance, indicating conserved and positive rol
266 her morpho-physiological traits related with drought tolerance.
267 is verified to play a negative role in plant drought tolerance.
268 growth rates as expected by a trade-off with drought tolerance.
269 onserved and positive roles of PTPN in plant drought tolerance.
270 which can facilitate fastidious discovery of drought tolerant genes leading to improved yield in pear
271 egetative and flowering stages of a terminal drought tolerant genotype, PRLT2/89-33, subjected to dro
272 een drought-sensitive (ICSB338) and enhanced drought-tolerant (SA1441) varieties.
273  STS dimension reflected segregation between drought-tolerant and waterlogging-tolerant species.
274                                  Moench.), a drought-tolerant C4 grass, contain up to 50 nodes and in
275 greenness and SPEI, while those dominated by drought-tolerant species showed weak covariance.
276         Surprisingly, neither immigrants nor drought-tolerant taxa had higher abundance in dispersal
277 rdinated shifts toward communities with more drought-tolerant traits driven by tree mortality, but th
278 mitation (within 24 h of re-watering) in the drought-tolerant variety, but recovery is impaired in th
279 g treatments, a well-watered treatment and a drought treatment in which plants were subjected to thre
280    However, the physiological linkages among drought, tree defences, and insect outbreaks are still u
281 a juniper (Juniperus californica), examining drought vulnerability as a function of climate, litholog
282  subsurface processes explained variation in drought vulnerability within and across species at both
283 and other environmental stressors, including drought, warming and nutrient stress.
284                   Our findings indicate that drought was associated with measures of IPV towards wome
285 sture to demonstrate that the 2000-2018 SWNA drought was the second driest 19-year period since 800 C
286 0 to 2010, known as the "turn-of-the-century drought," was likely more severe than any in the instrum
287  most extensive database available on shade, drought, waterlogging and cold tolerance for 799 norther
288 warming-amplified beetle life cycles whereas drought-weakened host defenses appear to have been a dis
289 r plants are not able to recover from severe drought when they have used up their elastic water stora
290 low capacity to reduce impact of the initial drought), while it is related to reduced recovery (low c
291 creased in the distal root orders exposed to drought, while the fiber-bound condensed tannnins increa
292 cultivation were initiated during periods of drought, with periods of forest recovery occurring durin
293 sult from additional reported occurrences of drought, with reported losses due to heat stress playing
294                     Our results suggest that drought, without mandatory water use restrictions, may c
295 uch as 23-33% below the field average during drought years and 26-33% during deluge years.
296 f pools with reduced or zero survival during drought years and a coincident increase in spatial varia
297 er growing, more stress-resistant species in drought years and/or chronically drier climate.
298 y of predicting the location of catastrophic drought years in advance.
299 at many pools sustain juvenile salmon in non-drought years transition into ecological traps during dr
300 olism is a major cause of plant death during drought, yet the spread of embolism throughout the plant

 
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