ライフサイエンスコーパス: meter per second

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 e values for macroscopic steel sheets at 600 meters per second.

7 ocities on the surface vary from 3.1 to 17.2 meters per second.

8 ted anisotropically at velocities of tens of meters per second.

9 5 degrees of latitude and translates at 103 meters per second.

10 of the axially transmitted speed of sound in meters per second.

11 micrometers) and impact velocities up to 840 meters per second.

12 is electrical tree type to exceed 10 million meters per second.

13 d at impact velocities ranging from 26 to 97 meters per second (2-13.5 J).

14 fluxes (PPF, 400-2080 micromoles per square meter per second; 22-150 moles per square meter per day;

15 hurricanes that were more intense by 3 to 7 meters per second (5 to 12 percent) for wind speed and 7

16 nd a maximum wind speed of approximately 375 meters per second, a value that differs from both Hubble

17 s electron liquid is found to be ~0.1 square meters per second, an order of magnitude higher than tha

18 ncandescent (INC) at 5 micromoles per square meter per second and a control treatment of 12 hours lig

19 ous irradiation at 400 micromoles per square meter per second and under 12 hours irradiance and 12 ho

20 PPF (100, 200, and 400 micromoles per square meter per second) and two lamp types, metal halide and h

21 2.5-fold increase in major hurricanes (>/=50 meters per second), and a fivefold increase in hurricane

22 30 to 40 sverdrups (Sv) (1 Sv = 10(6) cubic meters per second), and it occurs mainly in subtropical

23 e, corresponding to a light velocity of 1600 meters per second, and a transparency of 40% that increa

24 fast-moving particles (V approximately a few meters per second) are aligned along the symmetry axes o

25 Median SWS measurements (in meters per second), as well as change in median SWS (med

26 and strong, reaching a sustained 190 to 200 meters per second at an altitude marked by a pressure of

27 lly increases and peaks at winds of about 32 meters per second before decreasing.

28 photon flux (PPF), 200 micromoles per square meter per second, but with phytochrome photoequilibrium

29 er second by 9.3% and that of running at 2.5 meters per second by 4.0% compared with locomotion witho

30 e metabolic rate of treadmill walking at 1.5 meters per second by 9.3% and that of running at 2.5 met

31 ilation from relative speeds of less than 10 meters per second by comparing two optical atomic clocks

32 ld increase from 5.1 +/- 1.9 to 10.3 +/- 2.0 meters per second by the late 21st century, with a remar

33 ate that a megaflood (greater than 220 cubic meters per second) carved the canyon about 45,000 years

34 tic photon flux of 200 micromoles per square meter per second cool-white fluorescent (CWF); (b) conti

35 re laboratory velocity of 15 plus or minus 1 meters per second, corresponding to a 406 plus or minus

36 mation of nanojets with velocities up to 400 meters per second, created by pressurized injection of f

37 12 hours light at 400 micromoles per square meter per second CWF and 12 hours dark.

38 CWF; (c) 12 hours 400 micromoles per square meter per second CWF plus 12 hours dim CWF at 5 micromol

39 nd; (d) 12 hours [400] micromoles per square meter per second CWF plus 12 hours dim incandescent (INC

40 F); (b) continuous 400 micromoles per square meter per second CWF; (c) 12 hours 400 micromoles per sq

41 12 hours dim CWF at 5 micromoles per square meter per second; (d) 12 hours [400] micromoles per squa

42 s 0.13 sverdrup (Sv) (1 Sv = 1 million cubic meters per second) during Heinrich event 4 and to averag

43 Lava erupted at rates exceeding 100 cubic meters per second, eventually covering 35.5 square kilom

44 adiation at 560 to 580 micromoles per square meter per second from either metalhalide (MH), high pres

45 hydraulic diffusivity of 2.4 x 10(-2) square meters per second implies a major role for water circula

46 ot spots develops vertical shear of up to 70 meters per second in the eastward wind, which can explai

47 a flow rates, modeled up to about 7400 cubic meters per second into a dike ~15-kilometers long, which

48 ter volume droplets at speeds of hundreds of meters per second into a thin layer of liquid ethane coa

49 circulation with a poleward flow of about 20 meters per second is also evident.

50 ed that a 1% increase in aortic arch PWV (in meters per second) is related to a 0.3% increase in subs

51 this work, were of the order of hundreds of meters per second, less than what has been observed in o

52 jump to a height of 1.5 meters-reaching a 12 meters per second (m/s) peak velocity, a 7.14 x 10(4) m/

53 Aalpha nerves were measured and expressed as meters per second (m/s).

54 imates of absolute river discharge (in cubic meters per second) may be derived solely from satellite

55 ies greater than the local zonal flow by 100 meters per second, much higher than predicted by models.

56 c waves travel through tissue at 1.5 x 10(3) meters per second, much slower than x-rays, allowing ult

57 The Fermi velocity of 4 x 10(5) meters per second obtained from these transport experime

58 ous irradiation of 400 micromoles per square meter per second of photosynthetic photon flux and inclu

59 the sea surface implying that several cubic meters per second of freshwater are discharged into the

60 network upstream, and approximately 10 cubic meters per second of seepage emanates from its vertical

61 require an average of about 15 x 10(6) cubic meters per second of Southern Ocean deep ventilation ove

62 ch suggest that no more than 5 x 10(6) cubic meters per second of ventilated deep water is currently

63 e decline in summer river flows (-4.14 cubic meters per second per year), which is more relevant than

64 07 hours implies a strong wind (+650 +/- 310 meters per second) proceeding eastward.

65 to 0.9 meter, average velocity 0.20 to 0.75 meter per second) required to transport the pebbles.

66 adiation at 200 or 400 micromoles per square meter per second resulted in severe stunting and leaf ma

67 uctuating surface winds of approximately 0.5 meter per second resulting from the combination of an ea

68 ravitational acceleration, g ~ 9.77 +/- 0.01 meters per second squared, in a rubidium ((87)Rb) atom s

69 Slip propagates at approximately 88 meters per second, suggestive of a shear wave traveling

70 weak, jetlike features, with amplitudes of 5 meters per second, that are associated with the sunspot

71 For winds between 20 and 48 meters per second, this coefficient initially increases

72 Group velocities as slow as 91 meters per second to as fast as -800 meters per second w

73 are in the range of 10(-10) moles per square meters per second, two orders of magnitude faster than b

74 SSP SWV (in meters per second) was prospectively assessed twice in 2

75 w as 91 meters per second to as fast as -800 meters per second were measured and attributed to the in

76 icating better performance), and gait speed (meters per second) were measured.

77 ion, and with a peak sliding velocity of 1.1 meters per second, which propagated toward the Kathmandu

78 r), was towed across the North Atlantic at 6 meters per second while undulating between the surface a

79 survive under 2000 microeinsteins per square meter per second with air, although they have less resis

80 echnique for air circulation, achieving >0.3 meters per second with a potential volumetric flow rate

81 g which surface slip velocity peaked at ~3.5 meters per second with passage of the rupture front.

82 eriod of observation by +/-5.7 x 10(6) cubic meters per second, with density-inferred and wind-driven

83 current-driven velocities in excess of 4300 meters per second-within ~10% of the relativistic limit-