ライフサイエンスコーパス: subsidence

1 de dryer via pole-ward expanding subtropical subsidence.

2 diments and reductions in human-induced land subsidence.

3 ecades, and is surrounded by a broad zone of subsidence.

4 ports their proposal that mantle flow drives subsidence.

5 f dynamical transports of methane and strong subsidence.

6 efore apparently driving present-day surface subsidence.

7 e-injection produces 12 mm yr-1 of long-term subsidence, accompanied by an unprecedented seasonal osc

8 en years post-fire, detected permafrost thaw subsidence across 34% of the burned tundra area studied,

9 they highlight both localized rates of high subsidence and a significant spatial variability in subs

10 ination of rising sea levels, ground surface subsidence and anthropogenic sediment trapping, and a su

11 inable in the long-term, and to help reverse subsidence and capture carbon (C) there is an interest i

12 e of organic soils has resulted in vast soil subsidence and contributed to increased atmospheric carb

13 Subsidence and deceleration occurred over the subsequent

14 ic carbon (OC) was promoted by high tectonic subsidence and fluvial sediment supply.

15 Both isostatic subsidence and frequent storms under the colder climatic

16 es in the Early Miocene was brought about by subsidence and glacial erosion in West Antarctica during

17 nd-use types can help reduce or reverse soil subsidence and reduce GHG emissions.

18 thane and forms as a result of stratospheric subsidence and the particularly cool conditions near the

19 Thaw-induced subsidence and the resulting inundation along this progr

20 These results imply that subsidence and thermokarst-associated increases in organ

21 northern hemisphere, initiating south-polar subsidence and winter polar vortex formation.

22 More seamounts, slower subsidence, and less dense mantle on the western flank s

23 h rates reaching 20 cm yr(-1) and cumulative subsidence as much as 155 cm.

24 Stratospheric subsidence at the edges of the disturbance produced "bea

25 ponents of relative sea-level change (mainly subsidence) can also be locally appreciable.

26 ed silicates yielding a load-bearing and low-subsidence composite.

27 ntinued to increase linearly, ground surface subsidence created saturated microsites and suppressed R

28 yedoma), accounting for ~50% of the detected subsidence, despite representing only 30% of the fire di

29 ant cells during flooding and directly after subsidence, during which the plant is confronted with hi

30 nce and a significant spatial variability in subsidence, emphasizing the need for further measurement

31 ess, with high seismicity, continuing uplift/subsidence episodes with movements of approximately 70 c

32 vidence for repeated late Holocene coseismic subsidence events.

33 Namibia, combined with estimates of thermal subsidence history, suggest that biological productivity

34 oximately 23 year data-span to quantify land subsidence in cropland areas.

35 ce long-lived coherent structures that cause subsidence in local regions, explaining the low cloudine

36 low-level cooling and anomalous atmospheric subsidence in response to positive vegetation greenness

37 Radar altimetry also reveals time-varying subsidence in the North China Plain consistent with the

38 ls that parts of New Orleans underwent rapid subsidence in the three years before Hurricane Katrina s

39 tionary wave propagation, leading to greater subsidence, less precipitation, and higher temperatures

40 s controlling elevation (sediment accretion, subsidence), mangrove replacement of salt marsh, with or

41 Here we present a new subsidence map for the city, generated from space-based

42 show that the ongoing uplift and peripheral subsidence may result from a large mid-crustal diapir fe

43 ame) system revealed a slow (heave) and fast subsidence mode and an unstable oscillatory mode, a moda

44 abilized system with a slow (heave) and fast subsidence mode, and a stable oscillatory mode.

45 coverage, and can provide long-term temporal subsidence monitoring capability.

46 Erosion and subsidence moved the shoreline of Banda Aceh inland up t

47 uption, the instrument also measured gradual subsidence of 1.4 metres over the next several days, ref

48 e rates reach 18 cm yr(-1) with a cumulative subsidence of 206 cm, which potentially could adversely

49 tes that this weakness could be explained by subsidence of a metre or more since their construction.

50 infected mice during a key period after the subsidence of acute malaria symptoms, but during which m

51 ed in phosphine gas, probably resulting from subsidence of air into the troposphere.

52 Our results illustrate the maintenance and subsidence of different IAVs within swine farrow-to-wean

53 The subsidence of liver damage in G133E virus-infected birds

54 ble mechanisms to explain the appearance and subsidence of Lyme neuritis are discussed.

55 ctic tundra fires may induce widespread thaw subsidence of permafrost terrain in the first seven year

56 influence of gravity, display predominantly subsidence of the basin side (fault hanging wall), with

57 OCT features unique in these areas included: subsidence of the outer plexiform layer (OPL) and inner

58 atancy in the shallow fault zone that causes subsidence of the surface.

59 antial diminution of this resource and rapid subsidence of the valley floor.

60 res when we account for post-glacial crustal subsidence of these sites over the course of the anomalo

61 c routes, but economic factors have led to a subsidence of this effort, which places society on the p

62 storage and release accompanying growth and subsidence of tropical peatlands are affected by climate

63 s showing similar subsidence rates and total subsidence of up to 27 cm since 1988.

64 nsive groundwater extraction is causing land subsidence of up to 3 cm/y as measured using satellite-b

65 ose to the rupture area that had experienced subsidence of up to about 4 centimetres during the earth

66 iated with ENSO events may lead to a reduced subsidence over the Indian region, thus favoring normal

67 Throughout 2010-2011, strengthening subsidence produced a mesospheric hot-spot and caused ex

68 The maximum subsidence rate in central Taiwan is 8 cm yr(-1).

69 At least 60% of the total subsidence rate occurs within the uppermost 5-10 m, whic

70 sient 3D aquifer simulations showing similar subsidence rates and total subsidence of up to 27 cm sin

71 Subsidence rates from TOPEX/POSEIDON, JASON-1, ENVISAT,

72 Near Hanford, California, subsidence rates reach 18 cm yr(-1) with a cumulative su

73 d human settlement and has since experienced subsidence rates that are among the highest in the world

74 ation change, vertical accretion and shallow subsidence rates.

75 mate, nutrient inputs, sediment delivery and subsidence rates.

76 ks arising from local human activities, land subsidence, regional water management, global sea-level

77 d, while both the equatorial and subtropical subsidence regions have become drier and less cloudy.

78 ng of ice-rich permafrost ground causes land subsidence, resulting in development of distinctive land

79 nfer that the observed pattern of uplift and subsidence results from variations in the movement of mo

80 aphic and meteorological effects and/or land subsidence that cause relative sea level to rise faster

81 ered by a feedback between ice melt-back and subsidence to O(10(10)) W, which is similar to observed

82 Ocean--driven by convection to the west and subsidence to the east--known as the Walker circulation.

83 formations indicates that mild pre-eruptive subsidence took place in the Wallowa Mountains, followed

84 islands above the rupture and a 1-meter-deep subsidence trough farther from the trench.

85 Subsidence was greatest in severely burned, ice-rich upl

86 Sedimentation and subsidence were hence in pace, with subtle facies change

87 evel rise results from a combination of land subsidence, which has long been known to be present in t

88 Sequential interferograms indicate that subsidence within the caldera migrated from one resurgen

89 deslip oscillatory motion from a first order subsidence yaw behavior.