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Notice of Funding Opportunities

Adaptation Sciences (AdSci) Program FY2024
NIDIS Coping with Drought: Building Tribal Drought Resilience with Support from the Inflation Reduction Act (IRA)
Climate Program Office (CPO), Climate Adaptation Partnerships Program FY2024
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Rainfall

Improving extreme rainfall predictions: the limits of high-resolution climate models

Arctic Ocean’s autumn cool down accelerates sea ice formation
Climate variability in North Atlantic to increase dramatically by mid-century
Deep ocean waters near Antarctica are changing and disrupting global ocean circulation
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A climatology of the California Current System from a network of underwater gliders

The California Current is a highly productive eastern boundary current that supports a diverse array of economically important marine wildlife and fisheries.

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Enhanced ocean boundary later observations on NDBC TAO moorings
An important pilot study will provide data for improving observations in the Tropical Pacific….
Sea level in Indian Ocean shows abrupt rise, new study says
A CPO-funded study was recently published in the Journal of Geophysical Research, showing an abrupt sea level rise in the northern Indian Ocean since 2003….
Updates to authoritative Atlantic Hurricane database
The official 1956 to 1960 hurricane season revisions—primarily from the master’s thesis research of Mr. Sandy Delgado—are now available in the HURDAT2 file on the…
(a) Correlation coefficient (r) between the April-May anomaly in downwelling all-wave radiative flux measured at Barrow and the sea ice concentration for the following September in each grid cell of HadISST, 1993-2014. Regions of negative correlation indicate that positive anomalies measured in spring at Barrow were followed by negative anomalies in sea ice concentration. Black dots mark grid cells where the correlation is statistically significant (p < 0.05). (b) Standard deviation in September mean sea ice concentration in each grid cell of the HadISST data set from 1993-2014. The yellow square in both panels is the location of Barrow. The dashed-black line in both panels is the 20% standard deviation contour line for sea ice concentration in panel (b).
The role of springtime Arctic clouds in determining autumn sea ice extent
A study funded by the CPO’s Climate Observation Division confirms previous research suggesting spring clouds may be influencing arctic sea ice concentrations in the fall….
Updating the most complete archive of surface marine observations
The National Centers for Environmental Information released the latest update of the International Comprehensive Ocean–Atmosphere Data Set….
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