Grace Hawthorne als Theodora, Rollenbild, London

Signatur des Originals: S 36/F08785

Grace Pedley, Rollenbild, Hüftbild, in: Joan of Arc

Signatur des Originals: S 36/F09498

(Table 1) GRACE-derived mass balance of the Greenland ice sheet 2002-2010

We re-evaluate the Greenland mass balance for the recent period using low-pass Independent Component Analysis (ICA) post-processing of the Level-2 GRACE data (2002-2010) from different official providers (UTCSR, JPL, GFZ) and confirm the present important ice mass loss in the range of -70 and -90 Gt/y of this ice sheet, due to negative contributions of the glaciers on the east coast. We highlight the high interannual variability of mass variations of the Greenland Ice Sheet (GrIS), especially the recent deceleration of ice loss in 2009-2010, once seasonal cycles are robustly removed by Seasonal Trend Loess (STL) decomposition. Interannual variability leads to varying trend estimates depending on the considered time span. Correction of post-glacial rebound effects on ice mass trend estimates represents no more than 8 Gt/y over the whole ice sheet. We also investigate possible climatic causes that can explain these ice mass interannual variations, as strong correlations between GRACE-based mass balance and atmosphere/ocean parallels are established: (1) changes in snow accumulation, and (2) the influence of inputs of warm ocean water that periodically accelerate the calving of glaciers in coastal regions and, feed-back effects of coastal water cooling by fresh currents from glaciers melting. These results suggest that the Greenland mass balance is driven by coastal sea surface temperature at time scales shorter than accumulation.

Global and Regional Sea level budget components from GRACE and radar altimetry (2002-2014)

This dataset contains the result of a joint least squares inversion of GRACE and altimetry data. The results are evaluated in terms of sea level change for the global ocean as well as dedicated areas. In addition, some auxiliary data is provided to enable reproducibility of the results in Rietbroek et al. 2016, and a google Earth kmz file is provided which visualizes the trends derived from the inversion results.

Desempenho, mortalidade e escore fecal de bezerros aleitados com diferentes dietas líquidas e terapias de reidratação quando acometidos por diarreias

O objetivo deste trabalho foi avaliar o efeito da utilização de sucedâneo lácteo com alto conteúdo proteico de origem vegetal no desempenho e saúde de bezerros, e avaliar métodos de reidratação para o tratamento de diarreias. No primeiro estudo foram utilizados 33 bezerros da raça Holandês distribuídos nos tratamentos: 1) Alto volume e baixa proteína (AV/BP): 8 litros, 21,4% PB; 2) Alto volume e alta proteína (AV/AP): 8 litros, 23,7% PB e 3) Baixo volume e alta proteína (BV/AP): 6 litros, 23,7% PB. Os bezerros foram alojados em abrigos individuais, com livre acesso a água e concentrado. Não houve efeito dos tratamentos para o desempenho animal (P>0,05). Os tratamentos AV/BP e AV/AP resultaram em maior consumo de sucedâneo (P<0,05), mas não afetaram o consumo de concentrado nem o consumo total (P>0,05). O escore fecal foi maior (P>0,05) para animais nos tratamentos AV/AP e BV/AP. Os animais nos tratamentos AV/BP permaneceram maior número de dias em diarreia (P<0,05), em comparação aqueles aleitados com BV/AP, os quais tiveram menos dias com vida (P<0,05). A concentração de lactato foi maior (P<0,05) para animais nos tratamentos AV/BP e AV/AP enquanto a concentração de proteína total foi maior (P<0,05) nos tratamentos AV/BP e BV/AP. Sucedâneos com elevado conteúdo de proteína de origem vegetal afetam negativamente o desempenho de bezerros podendo levar o animal a morte. No segundo estudo foram comparados três soluções de hidratação oral quanto a sua eficiência em repor eletrólitos e água, além de manter o desempenho de bezerros. Foram utilizados 42 bezerros mestiços Holandês-Jersey, distribuídos nos tratamentos: 1) Soro comum, 2) Glutellac® e 3) Soro comum + Aminogut®. Os animais foram aleitados com 4 L/d de sucedâneo lácteo até a oitava semana de vida quando foram desaleitados de forma abrupta. As terapias de reidratação foram oferecidas quando os animais apresentavam escore fecal >= 3 na escala de 1 a 5. Não houve efeito das terapias de reidratação no desempenho nem em metabólitos sanguíneos (P>0,05). O consumo voluntário de água foi maior para os animais reidratados com Glutellac®, mas o consumo total maior para os animais reidratados com Soro comum. As concentrações de HCO3 e Na+ foram maiores para os animais no tratamento Glutellac® (P=0,088 e P=0,073 respectivamente), sendo a concentração de glicose também afetada pelo protocolo de hidratação (P<0,05). A concentração de HCO3 aumentou do primeiro para o segundo dia, a de K+ e glicose diminuíram do primeiro para o segundo dia, enquanto que o Beecf teve um comportamento variável segundo a terapia de reidratação utilizada. Houve efeito da interação tratamento x dia de avaliação apenas para a concentração de BUN (P<0,05). O pH, a concentração de Na+ e Beecf foram maiores em animais mais velhos, enquanto K+, hematócrito e hemoglobina, foram menores (P<0,05). O consumo voluntário de água foi maior em animais reidratados com Glutellac®, o que junto com a simplicidade de uso, representam as principais vantagens deste método de reidratação.

Australian water mass variations from GRACE data linked to Indo-Pacific climate variability

Time-variable gravity data from the Gravity Recovery And Climate Experiment (GRACE) mission are used to study total water content over Australia for the period 2002–2010. A time-varying annual signal explains 61% of the variance of the data, in good agreement with two independent estimates of the same quantity from hydrological models. Water mass content variations across Australia are linked to Pacific and Indian Ocean variability, associated with El Niño-Southern Oscillation (ENSO) and the Indian Ocean Dipole (IOD), respectively. From 1989, positive (negative) IOD phases were related to anomalously low (high) precipitation in southeastern Australia, associated with a reduced (enhanced) tropical moisture flux. In particular, the sustained water mass content reduction over central and southern regions of Australia during the period 2006–2008 is associated with three consecutive positive IOD events.

Steric sea-level variations inferred from combined Topex/Poseidon altimetry and GRACE gravimetry

In this study, we propose to estimate the steric sea-level variations over a < 2-year period (April 2002 through December 2003) by combining global mean sea level (GMSL) based on Topex/ Poseidon (T/P) altimetry with time-variable geoid averaged over the oceans, as observed by the GRACE (Gravity Recovery and Climate Experiment) satellite. In effect, altimetry-derived GMSL changes results from two contributions: Steric (thermal plus salinity) effects due to sea water density change and ocean mass change due to water exchange with atmosphere and continents. On the other hand, GRACE data over the oceans provide the ocean mass change component only. The paper first discusses the corrections to apply to the GRACE data. Then the steric contribution to the GMSL is estimated using GRACE and T/P data. Comparison with available thermal expansion based on in situ hydrographic data is performed.

On the decorrelation filtering of RL05 GRACE data for global applications

In autumn 2012, the new release 05 (RL05) of monthly geopotencial spherical harmonics Stokes coefficients (SC) from GRACE (Gravity Recovery and Climate Experiment) mission was published. This release reduces the noise in high degree and order SC, but they still need to be filtered. One of the most common filtering processing is the combination of decorrelation and Gaussian filters. Both of them are parameters dependent and must be tuned by the users. Previous studies have analyzed the parameters choice for the RL05 GRACE data for oceanic applications, and for RL04 data for global application. This study updates the latter for RL05 data extending the statistics analysis. The choice of the parameters of the decorrelation filter has been optimized to: (1) balance the noise reduction and the geophysical signal attenuation produced by the filtering process; (2) minimize the differences between GRACE and model-based data; (3) maximize the ratio of variability between continents and oceans. The Gaussian filter has been optimized following the latter criteria. Besides, an anisotropic filter, the fan filter, has been analyzed as an alternative to the Gauss filter, producing better statistics.