In New York, the entire winter has been filled with weather advisories, along with freezing rain, decreased blood circulation, sleet, swipes right, unused gym memberships, compromised public transportation infrastructure, depression, lassitude, lonely gloves, too much binge-watching, opportunistic slush of a certain sentience and the first 2,000 words of novels in various states of abandonment.
It is well known that the heavy isotope contents (18O and 2H) of rain decrease with increasing altitude.
From early to late-successional stage, seed rain decreased in density, increased in per capita species richness, gradually changed in species composition, and became less aggregated spatially.
Water de-stratification in the wet season in all culture system types occurred earlier than in the dry and hot seasons; possibly because cold water from rain decreased surface water temperature, in turn, encouraging de-stratification.
Correspondingly, the median interval between days with >5 mm rain decreased, but it increased between days with >15 and >25 mm rain.
For others, it may come not as a torrent of water at all -- but as waves of more frequent and prolonged drought, as rains decrease and rivers dry up.
In some places, the impacts may come not as a torrent of water at all -- but as waves of more frequent and prolonged drought as rains decrease and rivers dry up.
θobs(t) increases sharply at rainfall events dependent on the amount of rain, and decreases exponentially after rainfall because of evapotranspiration and infiltration.
Moreover, the number of households using rain water decreased by about 40%.
Other negative feedback loops could arise via reduced rain (following decreased cloud formation) or higher evaporative demand, both leading to lower soil moisture and eventually lower gs (effect 2.2 in Fig. 2).
