Lia Marie Johnson born November 23, is an American actress, singer, and Internet personality known for appearing in various web series, including the Emmy-winning web series Kids React created by the Fine Brothers , and for her own vlogging and social media output. In a Adweek profile she was referred to as one of “10 of the biggest young stars on YouTube”. Johnson was born in Wahiawa, Hawaii. Her family eventually settled in California. Johnson’s YouTube account was created in , with videos uploaded by her mother which featured her performances at talent shows ,  and church recitals. In the aftermath of the initial series episodes, she was surprised by the phenomenon of strangers knowing her and approaching her as fans, and remarked “I think Kids React was my very first viral video, ‘cus everyone knew my name after that. In , Johnson was added to the recurring cast of the spin-off series Teens React , and in was moved again to the newly established YouTubers React , which featured herself and various well known YouTube personalities. The song was originally performed by singer Sam Smith. Johnson has also been featured on the covers of Adweek and BYou Magazine. She appeared in the music video for Post Malone ‘s single ” Go Flex “, which was released on April 28,
FSRH Clinical Guideline: Male and Female Sterilisation (September 2014)
Lia Marie Johnson born November 23, is an American actress, singer, and Internet personality known for appearing in various web series, including the Emmy-winning web series Kids React created by the Fine Brothers , and for her own vlogging and social media output. In a Adweek profile she was referred to as one of “10 of the biggest young stars on YouTube”. Johnson was born in Wahiawa, Hawaii.
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After disappearing from the spotlight last year, year-old YouTuber and singer Lia Marie Johnson reappeared online through Instagram Live on May 8 and 9. She was acting eerily different from her former self, leaving her fans concerned about her drug use, safety and mental health. The Kids React series features the Fine Brothers off-camera showing popular or viral videos, music and elements of pop culture to children and asking them questions about their reactions and opinions to the featured subject.
The Fine Bros would go on to feature Johnson in 42 other Kids React videos until when she graduated to another one of the React series, Teens React. The original Kids React series inspired Teens React, as well as the other series created by the FBE, and they all follow a similar format with different audiences.
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Long-term records of upper-atmosphere pressure and related circulation patterns are needed to assess potential drivers of past severe droughts and evaluate how future climate changes may impact hydroclimatic systems. Our results show extended time periods dominated by a set of persistent upper-air pressure patterns, providing insight into the atmospheric conditions leading to periods of sustained drought and pluvial periods in the preinstrumental past.
A striking shift from meridional to zonal flow occurred at the end of the Little Ice Age and was sustained for several decades. The position of the mid-latitude storm track, which represents the primary large-scale moisture-delivery pathway to North America, is closely connected to the strength and position of upper-atmosphere pressure features such as the Pacific subtropical high and the Aleutian low 1.
Shifts in the dominance of certain synoptic-scale atmospheric features have occurred over the instrumental period and influenced drought and flood regimes in western North America, including the early 20th century pluvial period and the devastating droughts of the s and s ref. Records from tree rings and other paleoclimate proxies have provided insight into the range of variability in the hydroclimatic system beyond the relatively short instrumental record.
One of the most important findings in water-limited western North America is that there have been periods of severe and sustained drought in the preinstrumental past exceeding known droughts from the instrumental record 6. The cause of these droughts is thought to be sustained shifts in moisture delivery processes linked to changes in ocean—atmosphere systems, particularly ENSO 6. Long-term pressure data derived from the tree-ring record can be used to extend our understanding of these shifts in moisture-delivery processes by allowing an assessment of the frequency and persistence of certain circulation patterns and their variability through time.
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workers were still infected up to January (SI Appendix, Fig. S2). firmed case in affected chiefdoms after 18 May , the onset date.
Interdecadal modes of tropical Pacific ocean-atmosphere circulation have a strong influence on global temperature, yet the extent to which these phenomena influence global climate on multicentury timescales is still poorly known. Here we present a 2,year, multiproxy reconstruction of western Pacific hydroclimate from two speleothem records for southeastern Indonesia. The composite record shows pronounced shifts in monsoon rainfall that are antiphased with precipitation records for East Asia and the central-eastern equatorial Pacific.
Our findings, together with climate model simulations, highlight the likelihood that century-scale variations in tropical Pacific climate modes can significantly modulate radiatively forced shifts in global temperature. Meridional and zonal variations of the Indo-Pacific climate system have very different impacts on Earth’s climate.
Meridional shifts in the position of the ITCZ rapidly transmit hydroclimate perturbations across the hemispheres in response to changes in interhemispheric temperature gradients 1. By contrast, zonal shifts in the PWC, which alter the trade wind fields and the location and strength of deep convection both zonally and meridionally , extend the geographic reach of ENSO and contribute to global temperature changes 2 , 3 , 4.
Therefore, unravelling the history of deep atmospheric convection in the western equatorial Pacific region before instrumental measurements is critical for understanding the role of the tropics in modulating both regional and global climate variability. However, the influence of zonal displacements in deep convection associated with ENSO in driving tropical climate is implicated by other studies 9 , As a result, there are different hypotheses regarding the precise drivers of tropical Pacific hydroclimate over the past millennium, and the relative importance of meridional forcing from the extratropics versus zonal ENSO-like shifts inherent to the tropics.
These data reveal substantial changes in AISM rainfall and deep atmospheric convection at the ascending limb of the PWC over the past two millennia. Comparison of our results with coupled general circulation model CGCM simulations reveal century-scale periods of divergence between the paleodata and model simulations, highlighting a deficiency in the models to capture the lower-frequency variability of the PWC. As such, the influence of the PWC to amplify the radiatively forced warming and cooling trends of the past millennium is limited in the models.
Apostolia M. Tsimberidou, M.D., Ph.D.
Auxinic herbicides, mechanisms of action, and weed resistance: A look into recent plant science advances. Auxin governs dynamic cellular processes involved at several stages of plant growth and development. In this review, we discuss the mechanisms employed by auxin in light of recent scientific advances, with a focus on synthetic auxins as herbicides and synthetic auxin resistance mechanisms.
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Here we show, using a new high-resolution simulation of the realistic North Pacific Ocean, that ocean eddies are instead sustained by a different process that involves small-scale mixed-layer instabilities set up by large-scale atmospheric forcing in winter. This leads to a seasonal evolution of the eddy kinetic energy in a very large part of this ocean, with an amplitude varying by a factor almost equal to 2.
Perspectives in terms of the impacts on climate dynamics and future satellite observational systems are briefly discussed. As such, it is driven by nonlinear scale interactions that can transfer energy upscale or downscale. KE associated with mesoscale eddies is monitored from space by satellite altimeters and these eddies are also explicitly resolved in present-day realistic ocean numerical simulations.
Until recently, the broadly accepted paradigm is that these eddies are generated and sustained by the instability of the large-scale vertical current shear or horizontal gradient of quasigeostrophic potential vorticity QGPV in the ocean interior.
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