This document is a compilation of flood resistant provisions, prepared by the Federal Emergency Management Agency (FEMA), of the 2015 I-Codes (IBC, IRC, IEBC, IMC, IPC, IFGC, IFC, ISPSC, IPSDC, ICC-PC). Also included, as a separate document, is a summary of changes from the 2012 I-Codes.
General References on the 1% (100-year) flood standard:
See Also: What is a 100/500/1000-Year Flood Event?
This started the 100 year rain event system. Although it was never intended to be about flooding, the notion of a 100 year event was later incorporated into the NFIP when it was passed in 1968.
The record of Mississippi River floods goes back to the earliest explorers: High Flows and Flood History on the Lower Mississippi River Below Red River Landing, LA (1543 – Present) and the paleoclimate records show megafloods greatly exceeding even the 1927 flood: , , and (1999), Marine evidence for episodic Holocene megafloods in North America and the northern Gulf of Mexico, Paleoceanography, 14(4), 498–510, doi:10.1029/1999PA900017; and Tripsanas, E.K. et al., 2013. Paleoenvironmental and paleoclimatic implications of enhanced Holocene discharge from the Mississippi River based on the sedimentology and geochemistry of a deep core (JPC-26) from the Gulf of Mexico. Palaios, 28(9), pp.623–636.
This is a project to develop off-shore wind off Cape Cod. It’s relevance to the Louisiana Coast is that the appeals court ruled that the EIS was incomplete because there was not sufficient geological information about the sea bottom and whether it could support the structures.
Chris McLindon, Causes of Accelerated Wetlands Loss in the Late 20th Century – Southeast Louisiana (2016)
Kolker et al. (2011) found a tight coupling between patterns of land loss measured in the Barataria Basin by Couvillion et al. (2011) and their interpretation of subsidence from the historical record of the Grand Isle tidal gauge.
Damage from hurricanes is expected to increase significantly in the coming decades because of the effects of climate change and coastal development. In turn, potential requests for federal relief and recovery efforts will increase as well.
GMACCC Publishes “Climate Change & Security In South Asia: Cooperating For Peace”
A GMACCC report published on 31 May 2016 warns that a recent drought in India which has affected over 330 million people – causing displacement and threatening farms –is just the first hint of how climate change could destabilise the South Asian region, unless steps are taken to address the threat posed by a warming, resource-scarce world.
This Hurricane Surge Hazard Primer summarizes important basic technical information about surge phenomena, hazard, and risk. It provides an overview of surge hazard analysis, including uncertainty in surge hazard estimates. Importantly, this Primer describes the limitations of hurricane surge hazard analysis and risk management under the National Flood Insurance Program. The reader is encouraged to refer to other reports listed in the References for a more detailed explanation of many key concepts.
This is a more technical account of the specific issues of surge in the Pontchartrain basin:
Analysis of time-lapse dynamics of recently simulated major storm surges and historical storm surge maximum observations shed new light on spatial and temporal patterns of storm surge within the Lakes Pontchartrain and Maurepas region (PMSC region, see Figure 1). While the terms tilting or sloshing have been previously used to describe key dynamic processes of storm surge movement in Lake Pontchartrain, these terms can be misleading because the peak surge generally rotates around the lake perimeter (“surge rotation”) rather than directly transferring (tilting/sloshing) from one end of the lake to the other.
In this analysis, two recent storms are examined as archetypical events that exemplify a new conceptual model that we introduce. Hurricanes Katrina (2005) and Isaac (2012) had fundamentally different tracks which seem to illustrate well the contrasting patterns of storm surge rotation introduced here. However, while these exemplify a generalized surge rotation model, it is important to keep in mind that our conceptual model is built around local forcing on storm surge and not the larger coastal processes. Every storm is different and the resulting surge is always a result of regional and local forcing. The limitation of this study is that we only discuss the movement of surge within the PMSC region and not the dynamics of surge entering into the PMSC region by more regional meteorological or coastal processes. In spite of this limitation, much can be said about the generalized relative movement of maximum surge in the PMSC region