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Download PDF by Diego Fernández-Prieto, Roberto Sabia: Remote Sensing Advances for Earth System Science: The ESA

By Diego Fernández-Prieto, Roberto Sabia

To greater comprehend a number of the procedures and interactions that govern the Earth process and to figure out no matter if contemporary human-induced alterations may perhaps finally de-stabilise its dynamics, either common approach variability and the implications of human actions must be saw and quantified. during this context, the eu area service provider (ESA) released in 2006 the record “The altering Earth: New clinical demanding situations for ESA's residing Planet Programme” because the major motive force of ESA’s new Earth commentary (EO) technological know-how process. The rfile outlines 25 significant medical demanding situations protecting the entire diverse elements of the Earth procedure, the place EO know-how and ESA missions may supply a key contribution. during this framework, and aiming at improving the ESA medical aid in the direction of the fulfillment of “The Challenges”, the employer has introduced in 2008 a brand new initiative – the altering Earth technological know-how community – to aid younger scientists to adopt modern study actions contributing to accomplish the 25 medical demanding situations of the LPP through maximising using ESA facts. The initiative is applied via a couple of study tasks proposed and led through early-stage scientists at post-doctoral point for a interval of 2 years that are summarized during this SpringerBrief. those initiatives adopt leading edge study actions furthering into the main urgent problems with the Earth procedure, whereas exploiting ESA missions information with specified realization to the ESA information documents and the hot Earth Explorer missions.

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Additional resources for Remote Sensing Advances for Earth System Science: The ESA Changing Earth Science Network: Projects 2009-2011

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The systematic differences among the sensors have been carefully evaluated and discussed in Palazzi et al. [5]: in summary, they do not exceed 2° in the overlapping time period among all satellite sensors (2004–2005, dashed vertical lines in Fig. 2). The four sensors consistently reproduce the annual cycle of the subtropical barrier position, characterized by a wintertime shift of the barrier position toward the equator. The time series plotted in Fig. 2 (particularly at 600 K and 690 K) also clearly show a periodicity of approximately 2 years in the position of the subtropical barrier, which is ascribed to the impact of the quasi biennial oscillation (QBO) in the zonal mean zonal winds, the main source of interannual variability in the lower stratosphere.

Nature 249:810–812 18. Newman PA et al (2006) When will the Antarctic ozone hole recover? Geophys Res Lett 33:L12814 19. Papandrea E, Arnone E, Brizzi G, Carlotti M, Castelli E, Dinelli BM, Ridolfi M (2010) Twodimensional tomographic retrieval of MIPAS/Envisat measurements of ozone and related species. Int J Remote Sens 31(2):477–483 20. Premuda M, Masieri S, Bortoli D, Margelli F, Ravegnani F, Petritoli A, Kostadinov I, Giovanelli G, Cupini E (2009) A Monte Carlo simulation of radiative transfer in the atmosphere applied to ToTaL-DOAS.

During the SeaWiFS time period (Fig. 3b), the spring bloom was stronger than in the 1980s, and it extended further south than during the CZCS era, down to 54 E. Martinez et al. Fig. 3 Latitude versus time plots for the eastern Atlantic (average over 40°–0° W): ( a, b) Chl and (c, d) MLD during the CZCS (a, c) and Sea WiFS ( b, d) era. 6 mg m-3. They are reported on the MLD figures. The grey bars on the top of the figures correspond to the September-January time period (months of occurrence of the fall bloom) 36°–40° N.

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