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1  1 Sv = a flow of ocean water of 10(6) cubic meters per second).
2 y launch them at supersonic velocities (~400 meters per second).
3 accelerated within 1 second to speeds over 1 meter per second.
4 lipped episodically at rates averaging 0.002 meter per second.
5 c intensity of 200 microeinsteins per square meter per second.
6 ocities on the surface vary from 3.1 to 17.2 meters per second.
7 ted anisotropically at velocities of tens of meters per second.
8  5 degrees of latitude and translates at 103 meters per second.
9 e values for macroscopic steel sheets at 600 meters per second.
10 d at impact velocities ranging from 26 to 97 meters per second (2-13.5 J).
11  fluxes (PPF, 400-2080 micromoles per square meter per second; 22-150 moles per square meter per day;
12  hurricanes that were more intense by 3 to 7 meters per second (5 to 12 percent) for wind speed and 7
13 nd a maximum wind speed of approximately 375 meters per second, a value that differs from both Hubble
14 s electron liquid is found to be ~0.1 square meters per second, an order of magnitude higher than tha
15 ncandescent (INC) at 5 micromoles per square meter per second and a control treatment of 12 hours lig
16 ous irradiation at 400 micromoles per square meter per second and under 12 hours irradiance and 12 ho
17 PPF (100, 200, and 400 micromoles per square meter per second) and two lamp types, metal halide and h
18 2.5-fold increase in major hurricanes (>/=50 meters per second), and a fivefold increase in hurricane
19  30 to 40 sverdrups (Sv) (1 Sv = 10(6) cubic meters per second), and it occurs mainly in subtropical
20 e, corresponding to a light velocity of 1600 meters per second, and a transparency of 40% that increa
21 fast-moving particles (V approximately a few meters per second) are aligned along the symmetry axes o
22                  Median SWS measurements (in meters per second), as well as change in median SWS (med
23  and strong, reaching a sustained 190 to 200 meters per second at an altitude marked by a pressure of
24 lly increases and peaks at winds of about 32 meters per second before decreasing.
25 photon flux (PPF), 200 micromoles per square meter per second, but with phytochrome photoequilibrium
26 ilation from relative speeds of less than 10 meters per second by comparing two optical atomic clocks
27 ate that a megaflood (greater than 220 cubic meters per second) carved the canyon about 45,000 years
28 tic photon flux of 200 micromoles per square meter per second cool-white fluorescent (CWF); (b) conti
29 re laboratory velocity of 15 plus or minus 1 meters per second, corresponding to a 406 plus or minus
30 mation of nanojets with velocities up to 400 meters per second, created by pressurized injection of f
31  12 hours light at 400 micromoles per square meter per second CWF and 12 hours dark.
32  CWF; (c) 12 hours 400 micromoles per square meter per second CWF plus 12 hours dim CWF at 5 micromol
33 nd; (d) 12 hours [400] micromoles per square meter per second CWF plus 12 hours dim incandescent (INC
34 F); (b) continuous 400 micromoles per square meter per second CWF; (c) 12 hours 400 micromoles per sq
35  12 hours dim CWF at 5 micromoles per square meter per second; (d) 12 hours [400] micromoles per squa
36 adiation at 560 to 580 micromoles per square meter per second from either metalhalide (MH), high pres
37 hydraulic diffusivity of 2.4 x 10(-2) square meters per second implies a major role for water circula
38 ot spots develops vertical shear of up to 70 meters per second in the eastward wind, which can explai
39 circulation with a poleward flow of about 20 meters per second is also evident.
40 ed that a 1% increase in aortic arch PWV (in meters per second) is related to a 0.3% increase in subs
41  this work, were of the order of hundreds of meters per second, less than what has been observed in o
42 Aalpha nerves were measured and expressed as meters per second (m/s).
43 imates of absolute river discharge (in cubic meters per second) may be derived solely from satellite
44 ies greater than the local zonal flow by 100 meters per second, much higher than predicted by models.
45              The Fermi velocity of 4 x 10(5) meters per second obtained from these transport experime
46 ous irradiation of 400 micromoles per square meter per second of photosynthetic photon flux and inclu
47 network upstream, and approximately 10 cubic meters per second of seepage emanates from its vertical
48 require an average of about 15 x 10(6) cubic meters per second of Southern Ocean deep ventilation ove
49 ch suggest that no more than 5 x 10(6) cubic meters per second of ventilated deep water is currently
50  to 0.9 meter, average velocity 0.20 to 0.75 meter per second) required to transport the pebbles.
51 adiation at 200 or 400 micromoles per square meter per second resulted in severe stunting and leaf ma
52 uctuating surface winds of approximately 0.5 meter per second resulting from the combination of an ea
53          Slip propagates at approximately 88 meters per second, suggestive of a shear wave traveling
54 weak, jetlike features, with amplitudes of 5 meters per second, that are associated with the sunspot
55                  For winds between 20 and 48 meters per second, this coefficient initially increases
56               Group velocities as slow as 91 meters per second to as fast as -800 meters per second w
57 are in the range of 10(-10) moles per square meters per second, two orders of magnitude faster than b
58                                  SSP SWV (in meters per second) was prospectively assessed twice in 2
59 w as 91 meters per second to as fast as -800 meters per second were measured and attributed to the in
60 ion, and with a peak sliding velocity of 1.1 meters per second, which propagated toward the Kathmandu
61 r), was towed across the North Atlantic at 6 meters per second while undulating between the surface a
62 survive under 2000 microeinsteins per square meter per second with air, although they have less resis
63 eriod of observation by +/-5.7 x 10(6) cubic meters per second, with density-inferred and wind-driven

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