JPmia wrote:SFLcane wrote:toad strangler wrote:
OOF!
Yep...Let’s put this recurve discussion to bed now! This has been my concern to this point. Get ready folks

They're also mentioning that the high pressure pattern is a little further north than previous years.. anyone get that? and if so, let's discuss what that could mean.
Before we can discuss its location, let's first talk about what causes this high pressure area. Building off my previous post (
viewtopic.php?p=2807655#p2807655), we can see the natural currents of the Atlantic ocean transport warm water north, where it mixes with much colder water before remaining heat is released. When we have this colder water, it lowers sea-level and surface pressures. This causes compensating high pressure areas to form (generally to the north or to the south). Introducing...the Bermuda High. So what does a typical July pattern look like? Below is an example:

Now let's talk about the source of this ocean temperature difference. Fresh water deposits from Greenland runoff, glacial melt, and other sources of fresh water all play a major factor in this. Fresh water reduces the salinity in the ocean, which results in cold water having a higher buoyancy (i.e. it doesn't sink as quickly as the rate of warmer water). So let's do a quick recap. These aren't static features of course, but below is an overlay of current sea surface temperatures and some example features:

So now that we know a higher concentration of fresh water decreases SSTs and decreases SLP, and we know this correlates to compensating high pressure areas, how can we analyze this? One way is to use NSIDC data to analyze surface melt (
http://nsidc.org/greenland-today/greenl ... sis-tools/). Looking at 2020, there has been a recent spike in fresh water runoff:

While the atmosphere doesn't instantaneously respond to oceanic changes (these process are more gradual), we should start seeing a compensating high pressure area, which we are:

Now comparing this to my first image above, we can see this is currently displaced to the NW, in part due to the large baroclinic feature over NW Africa/Spain that has persisted for quite some time (which has accelerated the near historic SAL outbreak). If the CFS forecast is correct, we should be in a more traditional July setup by mid-July (although a bit zonal).

So we can also use this to explore how this impacts Atlantic hurricane tracks. An increase in fresh water will result in more ridging/a stronger area of high pressure. This increases the chance of U.S. strikes. Looking at recent active seasons with multiple U.S. strikes and their corresponding 500mb heights anomalies for those spikes:
2018
2005
2004

Some will probably remember the talk of the blocking Greenland high that causes Sandy's track, and this also coincided with historic surface melts in 2012 from July-September of that year:


While these certainly aren't the only influencing features and processes, it's one aspect that will influence steering currents as we head towards the heart of the hurricane season.