As soon as an iceberg calves, it starts to warm relative to its parent ice shelf.
The dust temperatures derived from far infrared fluxes are warm relative to spirals, ranging from 40 90 K.
Mean maximum daily stream temperatures ranged from 1.5 °C cooler to 1.0 °C warmer relative to pre-harvest years.
Ensemble pan-European projections under a 2 °C global warming relative to the preindustrial period reveal a more intense warming in south Eastern Europe by up to +3 °C, thus indicating that impacts of climate change will be disproportionately high for certain regions.
The observation model merged approaches suggest that the warmer sea surface and dryer FT relative to BL result in a less LCC, although the larger FT warming relative to BL enhances the LCC, resulting in a positive low cloud feedback.
Based on this terrestrial analogue, we develop a thermal model that consists of a thick insulating dusty layer over ice-saturated dust during a period of slight climatic warming relative to today's climate.
Not all cities show a warming relative to their rural surroundings.
The increase in thermal tolerance delays the bleaching threshold the longest in regions like Polynesia, where the models project lower warming relative to the global mean warming, as in [15].
The most recent arctic analysis [19] indicates that four of the five warmest decades of the past two millennia have occurred since 1950, and that recent summer temperatures are much as 1.4°C warmer relative to the long-term trend modulated by solar insolation.
Comparisons of different periods of the two forcing pathways suggest that the magnitude of aggregate climate change varies relatively linearly with the magnitude of global warming below approximately 2 °C of global warming (relative to the late-20th-century baseline).
