Qbo and its dependence on stratospheric resolution is. The quasibiennial oscillation in a double co2 climate by, kevin hamilton, yoshio kawatani, kevin hamilton and shingo watanabe year. Quasibiennial oscillation, layer of winds that encircle earths lower stratosphere, at altitudes from 20 to 40 kilometres about 12 to 25 miles, between latitudes 15 n and 15 s. Defined partially from wikipedia, the free encyclopedia. By yoshio kawatani, kevin hamilton, shingo watanabe, kevin hamilton and. They are alternately easterly and westerly, reversing about every months. Sensitivity of the qbo to mean tropical upwelling under a changing climate simulated with an earth system model.
Another important factor is the quasibiennial oscillation. Representation of the tropical stratospheric zonal wind in global. Raible1,3, stefan muthers1,3, julien anet4, eugene rozanov5,6, and werner schmutz6. Simulation of the stratospheric quasibiennial oscillation using a. Ccm,whichgeneratesitsown wind and temperature quasibiennial oscillation qbo, to study the effect of coupling on the qbo and to examine the qbo signals in stratospheric trace gases. The qbo period decreases in two parameterization setups by 30 %. As defined by a us national research council committee, a climate data record cdr is a time series of measurements of sufficient length, consistency and continuity to determine climate variability and change. The quasibiennial enso rhythm appears to be a harmonic oscillation in equatorial pacific atmosphereocean system, and it was in sync with the qbo in 187999 and 196383. Quasibiennial oscillation and tracer distributions in a coupled chemistryclimate model. High latitude blocking inrelation to the quasibiennial oscillation qbo the quasibiennial oscillation qbo is changes in equatorial zonal wind between easterlies and westerlies in the tropical stratosphere. Advancing the predictive capabilities of atmospheric general circulation models gcms necessitates a better understanding of the weatherclimate interface and, in particular, the impact of the stratosphere on tropospheric predictability. Giorgetta ma, doege mc 2005 sensitivity of the quasibiennial oscillation to co2 doubling. This study investigates the role of enso and the qbo on the frequency of ssws using the national center for atmospheric researchs whole atmosphere community climate model, version 3. Unprecedented atmospheric behaviour disrupts one of earth.
The quasibiennial oscillation in a double co2climate article pdf available in journal of the atmospheric sciences 682. These regular winds have been recorded since the 1950s and emerge from natural. The quasibiennial oscillation is the equatorial zonal wind between easterlies and westerlies in the tropical stratosphere with a period of 26 months on average. Predictability of the quasibiennial oscillation page 4. Some people consider heuristics to be wrong by definition, while others say they are correct until they stop. Many of the dynamical aspects of the qbo are best illustrated by a timeheight cross section of monthlymean equatorial zonal longitudinal wind plate 1. Since the qbo has a strong influence on the north atlantic oscillation and thereby north european weather, scientists speculated that. Results from the met o ce hadgem2ccs general circulation model are presented. Climateforced sealevel lowstands in the indian ocean during the last two millennia. The quasibiennial oscillations influence on lightning production and deep convection in the tropics.
Learn vocabulary, terms, and more with flashcards, games, and other study tools. The effects of anticipated twentyfirstcentury global climate change on the stratospheric quasibiennial oscillation qbo have been studied using a highresolution version of the model for interdisciplinary research on climate miroc atmospheric gcm. Modulation of the connection between boreal winter enso. The structure, dynamics, and ozone signal of the quasibiennial oscillation qbo produced by the 35yr nasa modernera retrospective analysis for research and applications, version 2 merra2, are examined based on monthly mean output. Atmosphereonly experiments in both present day and warmer climate. Quasibiennial oscillation of the stratosphere youtube. Wave driven circulation changes associated with the formation of 40hpa westward u. The sensitivity of the equatorial quasibiennial oscillation qbo to increasing. An unprecedented disruption of the atmospheric quasibiennial oscillation.
The influence of the quasibiennial oscillation on the troposphere. This phenomenon is sometimes referred to as the stratospheric quasibiennial oscillation to distinguish it from other atmospheric features that also have spectral peaks near two years. The quasibiennial oscillation is a regular feature of the climate system. Unprecedented atmospheric behavior disrupts one of earths most regular climate cycles. Song3 1goddard earth science technology and research gestar, morgan state university, baltimore, md, usa 2nasa goddard space flight center, greenbelt, md, usa. High above the equator winds slowly change from blowing eastward to westward and back again roughly every 28 months in a natural climate rhythm known as the quasibiennial oscillation qbo. Kawatani y, hamilton k, watanabe s 2011 the quasibiennial oscillation in a double co2 climate. The quasibiennial oscillation in a double co2 climate american.
The quasibiennial oscillation was the subject of a workshop in the canadian city of victoria from 16 to 18 march. A strange thing happened in the stratosphere a 60year pattern in the stratosphere changes up. Multidecadal variations of the effects of the quasi. Quasi biennial oscillation gravity waves parameterization climate change.
The model is the first version of the center for climate system researchnational. It may perhaps be natural to consider gravity waves as the main driving. Citeseerx document details isaac councill, lee giles, pradeep teregowda. However, when further 3yr running averages were evaluated and subtracted, qbo quasibiennial oscillations were noticed in all these parameters. The quasibiennial oscillation qbo, a quasiperiodic oscillation of easterly and westerly winds in the tropical stratosphere that is known to affect winter surface weather in the midlatitudes, is predictable several years into the future, according to a new modeling study by scaife et al. An unprecedented disruption of the atmospheric quasi. The quasibiennial oscillation qbo is a persistent, quasiperiodic, largeamplitude oscillation of the lowlatitude stratospheric circulation see baldwin et al. Quasibiennal oscillation qbo index formally known as singapore winds monthly since 1979. The waves driving the qbo range from large scale kelvin and. These tropical winds reverse their direction in a 26month cycle called the quasibiennial oscillation qbo. This disruption to the wind pattern called the quasi biennial oscillation did not have any immediate impact on weather or climate as we experience it on earths surface. This makes an easterly phase likely as we head into the winter of 201718.
Unprecedented atmospheric behaviour disrupts one of earths most regular climate cycles research science the normal flow of air high up in the atmosphere over the equator, known as the quasibiennial oscillation, was seen to break down earlier this year. Accompanying the zonal wind qbos are anomalies of temperature, trace constituents, and mean meridional circulation. It was first discovered in the late 1950s 1, 2 and features alternating eastward and westward windjets descending through the equatorial stratosphere, at roughly 1 km per month, from 50 km 3. The roles of equatorial trapped waves and internal inertiagravity waves in driving the quasibiennial oscillation. An unexpected disruption of the atmospheric quasibiennial.
Qbo variations in temperature and zonal wind were under. This quasibiennial oscillation qbo has been observed to dominate the winds in this region of the atmosphere for at least the last 6 decades and is characterized by a. Many of the dynamical as pects of the qbo are best illustrated by a timeheight cross section of monthlymean equatorial zonal longi tudinal wind plate 1. The quasibiennial oscillation qbo of zonal wind is a prominent mode of variability in the tropical stratosphere. The amplitude of the easterly phase is about twice as strong as that of the westerly phase. Sensitivity of the qbo to mean tropical upwelling under a. The quasibiennial oscillation in a double co2climate. The role of eddies in driving the tropospheric response to stratospheric heating. In order to simulate the quasibiennial oscillation qbo with a realistic period and amplitude, general circulation models commonly include parameterizations of small scale gravity waves gw. In the quadruped co2 simulations a reduction in qbo period of 14.
As noted above, the qbo is driven by the zonal mo mentum fluxes from. Accepted manuscript manuscripts that have been selected for publication. For climate graphics and access to data and links to other climate. A strange thing happened in the stratosphere eurekalert. However, the representation of stratospheric phenomena, including the tropical quasibiennial oscillation qbo and polar sudden stratospheric. From a fluid dynamical perspective, the qbo is a fascinating example of a. Tim stockdale, who represented ecmwf at the meeting, explains what the qbo is all about. They have not been typeset and the text may change before final.
A team of scientists has discovered an unexpected disruption in. Quasibiennial oscillation and tracer distributions in a coupled. Some of the variability does not appear to be caused systematically and occurs at random times. Quasibiennial oscillation and tracer distributions in a.
The quasibiennial oscillation qbo, is a quasiperiodic oscillation of the equatorial zonal wind. An assessment of the quasibiennial oscillation qbo and. The quasibiennial oscillation qbo dominates the variability of the equatorial stratosphere 1650 km and is easily seen as downward propagating easterly and westerly wind regimes, with a variable period averaging approximately 28 months. Quasibiennial oscillation in ionospheric parameters. Thats the definition of a heuristic, which can model a behavior but with no physical explanation. This oscillation is a manifestation of a downward propagation of winds with alternating sign. The quasibiennial oscillation qbo is a quasiperiodic oscillation of the equatorial zonal wind between easterlies and westerlies in the tropical stratosphere with a mean period of 28 to 29 months.
The quasibiennial oscillation qbo is a tropical lower stratospheric, downward propagating zonal wind variation, with an average period of. Quasibiennial oscillation an overview sciencedirect. Downward propagating easterly green and westerly red winds and their induced meridional circulation black contours with arrows for different phases of the qbo. Quasibiennial oscillation gravity waves parameterization climate. The influence of the stratospheric quasibiennial oscillation on trace gas levels at. Based on a preindustrial control run 1850, a 12 co2 run and a 4 x co2. The quasibiennial oscillation in a double co2 climate. A tenfold slowdown in river meander migration driven by plant life. Using 30 years of retrospective forecasts from the poama coupled model forecast system, we show that this. One involves the qbo modu lation of stratospheretroposphere exchange and, in particular, the ffux of air through the tropical. The qbo is most evident in the zonal mean zonal wind near the equator, which undergoes reversals from strong easterlies to strong westerlies through each qbo cycle, but has clear observable signals in. Unprecedented atmospheric behavior disrupts one of earths. The maddenjulian oscillation mjo during boreal winter is observed to be stronger during the easterly phase of the quasibiennial oscillation qbo than during the westerly phase, with the qbo zonal wind at 50 hpa leading enhanced mjo activity by about 1 month. The effects of wave driving are counteracted by mean upwelling, which acts to slow the qbo phase descent and lengthen the pe riod.
Effects of the stratospheric quasibiennial oscillation on longlived. Impact of the quasibiennial oscillation on predictability. Quasibiennial oscillation qbo anomalous change youtube. Such variability is called random variability or noise. Structure and dynamics of the quasibiennial oscillation. They blow at velocities of 15 to 35 metres per second about 35 to 80 miles per hour.
Climate variability is the term to describe variations in the mean state and other characteristics of climate such as chances or possibility of extreme weather, etc. Pdf the quasibiennial oscillation in a double co2climate. The quasibiennial oscillation in a double co2 climate core. When seasonal variations were eliminated by evaluating 12month running means, the ionospheric parameters foe, fof2 and hmf2 at juliusruh 54. The quasibiennial oscillation is fairly well simulated by use of a t21 60layer general. Hartmann department of atmospheric science, university of washington, seattle, washington. This exploratory study investigates its possible change by direct simulation of the qbo in a doubled co 2 climate for a range of gravity wave sources. An unexpected disruption of the atmospheric quasibiennial oscillation. Courtney schumacher variations in characteristics of tropical deep convection are examined for an. In this work, we explore how different gw parameterization setups determine the response of qbo properties to a warmer climate. Scientists and policymakers must acknowledge that carbon dioxide removal can be. Yoshio kawatani university of oxford department of physics. In the us, agencies such as nasa and noaa have sponsored operational and grant. The quasibiennial oscillation qbo of the equatorial lower and middle stratosphere is a fairly regular 2 to 3year cycle characterized by alternating descending regimes of easterly westward propagating and westerly eastward propagating zonal wind figure 1.
163 1648 766 464 427 1617 131 279 1263 587 1402 841 260 1197 794 1089 1209 1578 1117 724 1432 329 1316 736 378 48 1346 892 425 641 985 325 1343 862 1335 561 1192 206 1272 49 1292