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1 ion in direct flood damages during Hurricane Sandy.
2 areas of New York City affected by Hurricane Sandy.
3 areas of New York City affected by Hurricane Sandy.
5 y-5 displayed activities opposite to that of Sandy-2 by stimulating recombinant BAFF in vitro and end
6 B cells in vitro A single administration of Sandy-2 in mice induced B cell depletion within 2 weeks,
10 e clayey aggregates was 0.32, whereas in the sandy aggregates it was approximately 10 times lower.
11 A on (i) regional flood damages by Hurricane Sandy and (ii) local annual flood losses in Barnegat Bay
13 ity changes in sandbox experiments where two sandy and clayey soils were initially contaminated with
16 from four ponds were installed in a shallow sandy aquifer underlying a densely populated village and
18 rain of the Hermansky-Pudlak syndrome strain sandy, are abnormal, indicating that aberrant biogenesis
24 We collected 36 intertidal samples at 12 sandy beaches from four regions that spanned distances f
25 on invertebrate body sizes from a variety of sandy beaches in the UK to test the hypothesis that thes
27 karyotes are key ecosystem drivers in marine sandy beaches, an important and dynamic environment; how
29 s, descriptions or tags related to Hurricane Sandy bears a striking correlation to the atmospheric pr
31 proteins (pallidin, muted, cappuccino, HPS7/sandy); BLOC-2, consisting of HPS6/ruby-eye, HPS5/ruby-e
32 istical analysis of network dynamics, called SANDY, combining well-known global topological measures,
33 evee, while depositional features, such as a sandy crevasse-splay deposit are found further away from
35 investigate user attention to the Hurricane Sandy disaster in 2012, we analyze data from Flickr, a p
39 s a dynamic prealpine river with an alluvial sandy-gravel aquifer, which is characterized by short gr
40 t explain the broad geographic patterns, and sandy habitat best explains local patterns of movement.
41 harged from the river is present in both the sandy Holocene and gravelly Pleistocene aquifers and is
42 of firearm violence on school campuses since Sandy Hook and the ongoing toll on lives and health, the
43 gia basin, the New York Bight basin, and the Sandy Hook basin offer promising basalt-hosted reservoir
44 antially after the December 2012 shooting at Sandy Hook Elementary School in Newtown, Connecticut, wh
45 posure to the 9/11 terrorist attacks and the Sandy Hook School shootings were both significantly asso
47 was comparable to that in aggregates from a sandy, hydrocarbon-contaminated soil (~23%) scanned for
48 these areas, even though prior to Hurricane Sandy in 2012, no inlet was present in the eastern bay i
49 ce of additional flood events like Hurricane Sandy in recent centuries, and highlight the inadequacie
50 de of flooding in New York City by Hurricane Sandy is commonly believed to be extremely rare, with es
52 g Koc values for (14)C60 were equivalent for sandy loam and silt loam (3.55 log[mL/g]) but higher for
54 tify the prion adsorption capacity of whole, sandy loam soil (SLS) typically found in CWD endemic are
55 e (14)CO2 production in the silt loam or the sandy loam soil after 754 and 328 days, respectively, su
57 umber plants were cultivated for 150 days in sandy loam soil treated with 0 to 750 mg TiO2 NPs kg(-1)
58 ture grass (Paspalum notatum) was grown on a sandy loam soil while provided factorial additions of N
59 on of nAu was (i) greater on biochars than a sandy loam soil, (ii) greater at higher ionic strength a
60 )) derived from the natural dysbindin mutant Sandy mice, we have explored the role of dysbindin in do
64 liams, then at Oxford University with A.G. ("Sandy") Ogston, and finally back at Wisconsin with Willi
65 at start 4 weeks after landfall of Hurricane Sandy on October 29, 2012, and ending 2 years later, cre
66 arge-scale atmospheric patterns that steered Sandy onto the coast will become more frequent in the co
71 st unfavorable conditions were projected for Sandy Point where hatching success has already declined
72 conditions (Playa Grande, Pacific Ocean and Sandy Point, Caribbean Sea), but the effect varied in ar
75 eek and Still Creek-in northwestern Oregon's Sandy River Basin were monitored for temperature, dissol
76 a level rise, the return period of Hurricane Sandy's flood height decreased by a factor of approximat
77 over the 21st century is also accounted for, Sandy's return period is estimated to decrease by approx
78 persistence of the westward flow that led to Sandy's unprecedented track, implying that future atmosp
80 t sp. nov. were anchored within the shallow, sandy sea bed and lived in dense, typically monospecific
83 y 100% of TB transformed to TD except in the sandy sediment where 51-60% of 17alpha-TB was converted
84 icant for E2 in both sediments and TB in the sandy sediment with beta-isomers decaying more rapidly t
85 a marked impact on the surface charge of the sandy sediment, significantly affecting the mobility of
87 ea that grain-size disposition in subsurface sandy sediments drives the interstitial fluxes, influenc
88 creasing in concentration from the pristine, sandy sediments of Wells (ME), to industrially contamina
90 id Pleistocene sedimentation loads permeable sandy silt of Miocene age, successfully predicts the obs
92 ntration series of copper-paint contaminated sandy, silty-sand, and silty sediment types, DGT-probes
94 el of the snake enables the device to ascend sandy slopes close to the angle of maximum slope stabili
96 ken from a high-P clay-rich soil and a low-P sandy soil by combining advanced spectrometric and spect
97 d to two soils with contrasted properties: a sandy soil poor in organic matter and a clay soil rich i
98 upinus albus) grown in mesocosms filled with sandy soil results in a set of root architectural parame
102 correlate well with diesel removal from the sandy soil, but this is not the case with the clayey soi
103 nds were consistent with those measured in a sandy soil, except that the mobility of dissolved inorga
104 le influence on the ANPP-CO2 response on the sandy soil, possibly because Sorghastrum increased large
106 40, and 100 g kg(-1) of residual solids to a sandy soil, while experiment 2 investigated a loading ra
108 nation of rainfall (favoring grasses), soil (sandy soils favoring trees), and fire (limiting trees un
110 bsurface water with low hardness residing in sandy soils may have a higher potential of being contami
111 ffect size on finer textured soils, while on sandy soils the same increase in precipitation produced
113 y exceeds 20 cm in depth, especially in soft sandy substrates typical of Florida, making the great ma
116 vent-related potential assessment, Hurricane Sandy, the second costliest hurricane in United States h
117 we compare resultant deposition by Hurricane Sandy to earlier storm-induced flood layers in order to
118 riods affect U stability, we dosed saturated sandy wetland mesocosms planted with Scirpus acutus with
119 hat short periods of drought conditions in a sandy wetland, which expose reduced sediments to air, ma
120 We applied these strategies to Hurricane Sandy, which struck the northeastern United States in Oc
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