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It carries a highly optimistic energy, inspiring one to get going on manifesting one's One can actually create a 'mini-vortex' by arranging a group of Sedonalite.
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The interfaces include a bibliometric module that provides usage statistics based on article downloads and impact indicators based on citations. This allows for the following up of the performance of the collections and the individual journals, and contributes to the enhancement of the evaluation of scientific production. The SciELO Open Access collections represent an important global public good, contributing to the advancement of national programs and priorities on scientific research and communication.

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Between the ages of two and five, kids often use tactile forms of play to engage with the world around them. The geological designs are perfectly scaled for newcomers to the world of play. Whereas Labyrinth, Jet Dance, Race and Tide Pool take their cues from streams and sandy shorelines, Pico, Alto and Hop are inspired by mountains, volcanic formations and playful stepping stones. Want to see them in person? More details on all this below. But first—let's take a closer look at these unique formations! Pico is a mountainous play structure that sits 18 inches from surface level.

Wang, and G. Sun, Review and prospects of research on low vortex on the Qinghai-Tibetan plateau. Lu, J. China Meteorological Press, pp. Luo, S. Lutz, H. Inoue, and J.

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Machado, L. Rossow, R. Guedes, and A. Walker, Life cycle variations of mesoscale convective systems over the Americas. Maddox, R.

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McCann, D. Mecikalski, J.


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Bedka, S. Paech, and L. Litten, A statistical evaluation of GOES cloud-top properties for nowcasting convective initiation. Rosenfeld, and A. Manzato, Evaluation of geostationary satellite observations and the development of a 1—2 h prediction model for future storm intensity. Mills, P. Astling, Detection of tropopause penetrations by intense convection with GOES enhanced infrared imagery. Purdom, J. Rosenfeld, D. Lensky, Satellite-based insights into precipitation formation processes in continental and maritime convective clouds. Schmetz, J. Tjemkes, M.

Gube, and L. Schmidt, E. Arduini, B.

Wielicki, R. Stone, and S. Tsay, Considerations for modeling thin cirrus effects via brightness temperature differences. Bedka, D. Lindsey, A. Sokol, Z.

The Atom WAS Considered A Vortex By Mainstream Scientists | Unariun Wisdom

Wang, A-Train observations of deep convective storm tops. Shou, S. Li, and X. Yao, Mesoscale Meteorology. China Meteorological Press , pp. Siewert, C.


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Koenig, and J. Mecikalski, Application of Meteosat second generation data towards improving the nowcasting of convective initiation. Shen, and L. Kang, Mesoscale system study of extreme rainfall over Sichuan Basin in July Tao, S. Science Press, pp.

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Wang, P. Lyons, W. Schmid, and H. Lin, Further evidences of deep convective vertical transport of water vapor through the tropopause. Wang, X. Liao, A. Min, and C. Xiang, S. Li, D. Li, and S. Yang, An analysis of heavy precipitation caused by a retracing plateau vortex based on TRMM data. Xu, J. Guo, Q. Lu, F. Lu, and X. Zhang, Innovations in the data processing algorithm for Chinese FY meteorological satellites.

Xu, Y. Liu, and G. Xu, Introduction of Atmospheric Sciences. Nanjing University Press, pp.