Forecasting Global Temperature Variations by Neural Networks

Global temperature variations between 1861 and 1984 are forecast usingsregularization networks, multilayer perceptrons and linearsautoregression. The regularization network, optimized by stochasticsgradient descent associated with colored noise, gives the bestsforecasts. For all the models, prediction errors noticeably increasesafter 1965. These results are consistent with the hypothesis that thesclimate dynamics is characterized by low-dimensional chaos and thatsthe it may have changed at some point after 1965, which is alsosconsistent with the recent idea of climate change.s

Seasonal adjustment and cointegration

El documento examina el efecto de filtros de ajuste en el tamaño y poder de prueba de cointegración que usan los residuales como pruebas ADF y PP, mediante procedimientos MonteCarlo y una aplicación empírica. Nuestros resultados indican que el uso de filtros distorsiona el tamaño y reduce el poder de estas pruebas.

Ecologia demogràfica de la perca americana (Micropterus salmoides) a l'Estany de Banyoles

L'Estany de Banyoles, sistema peculiar tant des del punt de vista de la seva formació geològica com de les seves característiques limnològiques, conté actualment una comunitat de peixos profundament modificada respecte de la comunitat original. La perca americana (Micropterus salmoides), introduïda a finals dels anys seixanta del segle XX, és avui una de les espècies dominants en aquesta comunitat, i ocupa sobretot l'hàbitat litoral de l'Estany. Es tracta d'una espècie molt ben estudiada a Nord Amèrica des de diverses disciplines de la biologia i des de fa diverses dècades, cosa que ha comportat que actualment es disposi d'un gran volum d'informació sobre ella. Amb tot, fora del seu continent d'origen ha rebut poca atenció, malgrat l'amplia expansió que ha experimentat arreu del món. En aquesta tesi doctoral s'han abordat, amb un enfocament descriptiu, aspectes fins ara desconeguts per a l'espècie a l'Estany de Banyoles, a la península ibèrica i fins i tot a Europa. Concretament, se n'ha analitzat la condició, el creixement i la demografia, així com les seves variacions temporals. Amb aquesta finalitat, s'ha dissenyat un mostreig composat de deu campanyes de pesca intensives més alguns petits mostrejos addicionals intercalats, mostreig que s'ha allargat des del juliol del 1997 i fins el novembre del 1999. La captura dels exemplars s'ha realitzat mitjançant una tècnica de pesca elèctrica amb una embarcació posada a punt expressament per a aquest estudi, la qual s'ha mostrat considerablement eficient malgrat les dificultats que ofereix el medi. S'ha realitzat un mostreig de marcatge-recaptura basat en la mutilació d'aletes i, en alguns casos, en el marcatge amb pintura acrílica. Només en la darrera campanya (novembre del 1999) s'ha sacrificat una part important de les captures a fi de retirar-ne els otòlits per a la determinació de l'edat. Pel que fa a l'anàlisi de les dades, s'ha aplicat un ampli ventall de mètodes i models per a cada un dels aspectes estudiats, a fi de contrastar-ne els resultats i validar-ne la seva fiabilitat. En el cas de la condició, s'han aplicat mètodes d'anàlisi de la covariància (ANCOVA) i altres mètodes anàlegs, així com, paral·lelament, regressions i anàlisis derivades a partir de la relació longitud-pes. En l'estudi del creixement, s'han realitzat ajustaments de diversos models mitjançant regressions sobre dades de mida a l'edat i sobre dades d'increments de mida observats per interval de temps. També s'han aplicat anàlisis de freqüències de longitud, i, finalment, s'han aplicat mètodes de retrocàlcul a partir dels increments anuals del radi observats en els otòlits. Finalment, en el cas de l'estudi de la demografia, s'han aplicat models de marcatge-recaptura per a l'estimació de la grandària poblacional i de la supervivència, i, a més, s'han ajustat diversos models continus de supervivència sobre aquestes estimacions prèvies. També s'han estimat les capturabilitats associades a la nova tècnica de captura. Per una altra banda, s'ha implementat i realitzat un mostreig sobre la població de pescadors esportius de l'Estany encarat a determinar, bàsicament, la pressió de pesca a què es veu sotmesa l'espècie. Els resultats mostren sobretot una alta estabilitat interanual en tots els aspectes estudiats, que s'explica per l'estabilitat ambiental que, al seu torn, és característica d'aquest ecosistema lacustre. Això reverteix en una longevitat màxima observada que iguala la màxima descrita a la literatura per a l'espècie. Alhora, també s'han descrit fortes oscil·lacions estacionals tant en la condició, com en el creixement, com també en la supervivència, les quals, però, presenten certes diferències en la seva temporalitat, cosa que indica una certa diferenciació en els factors que les regulen.

Nonbreeding-Season Drivers of Population Dynamics in Seasonal Migrants: Conservation Parallels Across Taxa

For seasonal migrants, logistical constraints have often limited conservation efforts to improving survival and reproduction during the breeding season only. Yet, mounting empirical evidence suggests that events occurring throughout the migratory life cycle can critically alter the demography of many migrant species. Herein, we build upon recent syntheses of avian migration research to review the role of non-breeding seasons in determining the population dynamics and fitness of diverse migratory taxa, including salmonid fishes, marine mammals, ungulates, sea turtles, butterflies, and numerous bird groups. We discuss several similarities across these varied migrants: (i) non-breeding survivorship tends to be a strong driver of population growth; (ii) non-breeding events can affect fitness in subsequent seasons through seasonal interactions at individual- and population-levels; (iii) broad-scale climatic influences often alter non-breeding resources and migration timing, and may amplify population impacts through covariation among seasonal vital rates; and (iv) changes to both stationary and migratory non-breeding habitats can have important consequences for abundance and population trends. Finally, we draw on these patterns to recommend that future conservation research for seasonal migrants will benefit from: (1) more explicit recognition of the important parallels among taxonomically diverse migratory animals; (2) an expanded research perspective focused on quantification of all seasonal vital rates and their interactions; and (3) the development of detailed population projection models that account for complexity and uncertainty in migrant population dynamics.

Contrasting Seasonal Survivorship of Two Migratory Songbirds Wintering in Threatened Mangrove Forests

Long-distance migrants wintering in tropical regions face a number of critical conservation threats throughout their lives, but seasonal estimates of key demographic parameters such as winter survival are rare. Using mist-netting-based mark-recapture data collected in coastal Costa Rica over a six-year period, we examined variation in within- and between-winter survivorship of the Prothonotary Warbler (Protonotaria citrea; 753 young and 376 adults banded), a declining neotropical habitat specialist that depends on threatened mangrove forests during the nonbreeding season. We derived parallel seasonal survivorship estimates for the Northern Waterthrush (Seiurus noveboracensis; 564 young and 93 adults banded), a cohabitant mangrove specialist that has not shown the same population decline in North America, to assess whether contrasting survivorship might contribute to the observed differences in the species’ population trajectories. Although average annual survival probability was relatively similar between the two species for both young and adult birds, monthly estimates indicated that relative to Northern Waterthrush, Prothonotary Warblers exhibited: greater interannual variation in survivorship, especially within winters; greater variation in survivorship among the three study sites; lower average between-winter survivorship, particularly among females, and; a sharp decline in between-winter survivorship from 2003 to 2009 for both age groups and both sexes. Rather than identifying one seasonal vital rate as a causal factor of Prothonotary Warbler population declines, our species comparison suggests that the combination of variable within-winter survival with decreasing between-winter survival demands a multi-seasonal approach to the conservation of this and other tropical-wintering migrants.

Climate response to basin-scale warming and cooling of the North Atlantic Ocean

Using experiments with an atmospheric general circulation model, the climate impacts of a basin-scale warming or cooling of the North Atlantic Ocean are investigated. Multidecadal fluctuations with this pattern were observed during the twentieth century, and similar variations--but with larger amplitude--are believed to have occurred in the more distant past. It is found that in all seasons the response to warming the North Atlantic is strongest, in the sense of highest signal-to-noise ratio, in the Tropics. However there is a large seasonal cycle in the climate impacts. The strongest response is found in boreal summer and is associated with suppressed precipitation and elevated temperatures over the lower-latitude parts of North and South America. In August­-September-­October there is a significant reduction in the vertical shear in the main development region for Atlantic hurricanes. In winter and spring, temperature anomalies over land in the extratropics are governed by dynamical changes in circulation rather than simply reflecting a thermodynamic response to the warming or cooling of the ocean. The tropical climate response is primarily forced by the tropical SST anomalies, and the major features are in line with simple models of the tropical circulation response to diabatic heating anomalies. The extratropical climate response is influenced both by tropical and higher-latitude SST anomalies and exhibits nonlinear sensitivity to the sign of the SST forcing. Comparisons with multidecadal changes in sea level pressure observed in the twentieth century support the conclusion that the impact of North Atlantic SST change is most important in summer, but also suggest a significant influence in lower latitudes in autumn and winter. Significant climate impacts are not restricted to the Atlantic basin, implying that the Atlantic Ocean could be an important driver of global decadal variability. The strongest remote impacts are found to occur in the tropical Pacific region in June­-August and September­-November. Surface anomalies in this region have the potential to excite coupled ocean­atmosphere feedbacks, which are likely to play an important role in shaping the ultimate climate response.

The effect of doubled CO2 and model basic state biases on the monsoon-ENSO system. I: Mean response and interannual variability

The impact of doubled CO2 concentration on the Asian summer monsoon is studied using a coupled ocean-atmosphere model. Both the mean seasonal precipitation and interannual monsoon variability are found to increase in the future climate scenario presented. Systematic biases in current climate simulations of the coupled system prevent accurate representation of the monsoon-ENSO teleconnection, of prime importance for seasonal prediction and for determining monsoon interannual variability. By applying seasonally varying heat flux adjustments to the tropical Pacific and Indian Ocean surface in the future climate simulation, some assessment can be made of the impact of systematic model biases on future climate predictions. In simulations where the flux adjustments are implemented, the response to climate change is magnified, with the suggestion that systematic biases may be masking the true impact of increased greenhouse gas forcing. The teleconnection between ENSO and the Asian summer monsoon remains robust in the future climate, although the Indo-Pacific takes on more of a biennial character for long periods of the flux-adjusted simulation. Assessing the teleconnection across interdecadal timescales shows wide variations in its amplitude, despite the absence of external forcing. This suggests that recent changes in the observed record cannot be distinguished from internal variations and as such are not necessarily related to climate change.

On the natural variability of the pre-industrial European climate

We suggest that climate variability in Europe for the “pre-industrial” period 1500–1900 is fundamentally a consequence of internal fluctuations of the climate system. This is because a model simulation, using fixed pre-industrial forcing, in several important aspects is consistent with recent observational reconstructions at high temporal resolution. This includes extreme warm and cold seasonal events as well as different measures of the decadal to multi-decadal variance. Significant trends of 50-year duration can be seen in the model simulation. While the global temperature is highly correlated with ENSO (El Nino- Southern Oscillation), European seasonal temperature is only weakly correlated with the global temperature broadly consistent with data from ERA-40 reanalyses. Seasonal temperature anomalies of the European land area are largely controlled by the position of the North Atlantic storm tracks. We believe the result is highly relevant for the interpretation of past observational records suggesting that the effect of external forcing appears to be of secondary importance. That variations in the solar irradiation could have been a credible cause of climate variations during the last centuries, as suggested in some previous studies, is presumably due to the fact that the models used in these studies may have underestimated the internal variability of the climate. The general interpretation from this study is that the past climate is just one of many possible realizations and thus in many respects not reproducible in its time evolution with a general circulation model but only reproducible in a statistical sense.